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Earth Science Frontiers, 22(1): 88–101 (in Chinese with English Abstract)",{"EN":557},"The Yinggehai Basin is a unique NNW-trending petroliferous basin in the northwestern South China Sea. This paper mainly utilized stratigraphic, tectonic and seismic data by characterizing the geological structures and conducting the geo-mechanical analysis to study the formation, evolution and dynamics of the Yinggehai Basin. The study indicates that the Ailaoshan-Truong Son extruded terrane is composed of multiple secondary extruded bodies. The Red River fault zone, located within the Qiangtang-Simao-Yinggehai mantle flow channel and basin zone, experienced transform-type sinistral strike-slip motion before the basin forming stage and formed a NW-trending extruded mantle uplift, which activated the Yinggehai basin. After experiencing the rift depression, fault depression, and fault subsidence, the basin eventually formed large-scale, thick sedimentation features with ideal hydrocarbon-forming conditions at the end of the Miocene. Later, the basin dynamically transformed and entered a period of tectonic superposition, reworking, and thermal subsidence. Superposition of the NNW thrust sinistral strike-slip fault zone on the northern Hanoi sub-basin complicated the basin structure. Since the Pliocene, the southern Yinggehai main basin has been transformed into an extensional dextral strike-slip environment that hosted numerous mud diapirs. The thin crust and high geothermal gradient provide favorable conditions for the large-scale accumulation of natural gas.",{"EN":559},"Geological Structure and Dynamics of the Yinggehai Active Rift Basin, South China Sea",{"VOID":561},"10.1007\u002Fs12583-021-1405-3","VERIFIED","Auto Verify","https:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs12583-021-1405-3",[566,584,601,628,643],{"id":567,"sortIndex":568,"researcher":20,"roles":569,"affiliations":571,"properties":581},"7a466e3b-b72f-4966-a980-0c5be7cab6dd",4,[570],"AUTHOR",[572],{"id":20,"sortIndex":21,"affiliation":573,"properties":20},{"id":574,"createTime":575,"updateTime":575,"relativeEntities":576,"slug":577,"properties":578,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"72904fc0-c3bc-4964-a98d-651fb6ebe56d","2024-04-20T15:31:22.199+00:00",[],"Zhanjiang-Branch-of-CNOOC-Ltd-Zhanjiang-China",{"title":579},{"EN":580},"Zhanjiang Branch of CNOOC Ltd., Zhanjiang, China",{"title":582},{"VI":583},"Shenglin He",{"id":585,"sortIndex":52,"researcher":20,"roles":586,"affiliations":587,"properties":598},"496bac92-1ad7-48a6-8401-b8d30b8cda26",[570],[588],{"id":20,"sortIndex":21,"affiliation":589,"properties":20},{"id":590,"createTime":591,"updateTime":592,"relativeEntities":593,"slug":594,"properties":595,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"0a54bc8d-dd4c-47ce-be24-c10753353637","2024-04-21T09:55:30.553+00:00","2025-06-11T23:14:39.784+00:00",[],"School-of-Earth-Resources-China-University-of-Geosciences-Wuhan-China",{"title":596},{"EN":597},"School of Earth Resources, China University of Geosciences, Wuhan, China",{"title":599},{"VI":600},"Xiaobo Zhao",{"id":602,"sortIndex":21,"researcher":20,"roles":603,"affiliations":604,"properties":625},"d28a0dcc-aa0e-4f1a-a171-0b3c6a9af2d0",[570],[605,615],{"id":20,"sortIndex":21,"affiliation":606,"properties":20},{"id":607,"createTime":608,"updateTime":609,"relativeEntities":610,"slug":611,"properties":612,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"bc770b47-edc9-46ac-80b5-57acde458180","2023-12-11T12:34:15.531+00:00","2024-10-03T08:44:57.415+00:00",[],"College-of-Environmental-Science-and-Engineering-Tongji-University-Shanghai-China",{"title":613},{"VI":614},"College of Environmental Science and Engineering, Tongji University, Shanghai, China",{"id":616,"sortIndex":206,"affiliation":617,"properties":624},"60c4e3a4-8a8d-4578-af2e-ef43e4137592",{"id":618,"createTime":619,"updateTime":619,"relativeEntities":620,"slug":20,"properties":621,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"628b26a6-7dd0-4859-bf1f-6ca7d2ddd3a1","2023-12-13T11:50:49.894+00:00",[],{"title":622},{"VI":623},"The Administrative Centre for China’s Agenda 21 (ACCA21), Beijing, China",{},{"title":626},{"VI":627},"Yue Yao",{"id":629,"sortIndex":206,"researcher":20,"roles":630,"affiliations":631,"properties":640},"f62dd05f-dbeb-4a75-8cb4-1e40fde09d7e",[570],[632],{"id":20,"sortIndex":21,"affiliation":633,"properties":20},{"id":634,"createTime":635,"updateTime":635,"relativeEntities":636,"slug":20,"properties":637,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"a9a1a17a-2d6b-4c65-9b65-80ac0826f4b3","2023-12-27T17:32:08.082+00:00",[],{"title":638},{"VI":639},"School of Energy Resources, China University of Geosciences (Beijing), Beijing, China",{"title":641},{"VI":642},"Shaobin Guo",{"id":644,"sortIndex":142,"researcher":20,"roles":645,"affiliations":646,"properties":655},"ffdd974d-bcec-4ff2-a4e3-760e550e5a30",[570],[647],{"id":20,"sortIndex":21,"affiliation":648,"properties":20},{"id":649,"createTime":650,"updateTime":650,"relativeEntities":651,"slug":20,"properties":652,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"cc589e0f-c465-4ef3-b2d2-5a4484990691","2023-12-13T11:50:49.913+00:00",[],{"title":653},{"VI":654},"School of Earth Sciences and Spatial Information Engineering, Hunan University of Science and Technology, Changsha, China",{"title":656},{"VI":657},"Xiaopeng Li",{"url":564,"publisher":659,"properties":687},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":660,"slug":10,"properties":661,"entityType":18,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21,"subjectFields":665,"manageAffiliations":666,"indexDatabases":667,"url":93,"thumbnailPath":20,"statistic":682,"gsStatistic":20,"type":160,"analyzePriority":20},[],{"issn":662,"eissn":663,"title":664},{"VOID":13},{"VOID":15},{"EN":17},[],[],[668,675],{"id":75,"indexDatabase":669,"url":88,"indexYears":89,"academicFieldIds":674,"indexDatabaseRanking":92},{"id":77,"createTime":78,"updateTime":79,"relativeEntities":670,"label":671,"description":672,"key":85,"publicationTags":673,"standard":20},[],{"EN":82,"VI":82},{"EN":82,"VI":84},[87],[91],{"id":56,"indexDatabase":676,"url":71,"indexYears":20,"academicFieldIds":681,"indexDatabaseRanking":20},{"id":58,"createTime":59,"updateTime":60,"relativeEntities":677,"label":678,"description":679,"key":67,"publicationTags":680,"standard":20},[],{"EN":63,"VI":63},{"VI":65,"EN":66},[69,70],[73],{"impactFactor":21,"impactFactorByYear":683,"i10Index":108,"i10IndexLast5Year":109,"totalPublication":110,"totalPublicationByYear":684,"totalCitation":128,"totalCitationByYear":685,"totalCitationPerPublication":143,"totalCitationPerPublicationByYear":686,"hindexLast5Year":127,"hindex":127},{"2012":96,"2013":97,"2014":98,"2015":99,"2016":100,"2017":101,"2018":102,"2019":103,"2020":104,"2021":105,"2022":106,"2023":107},{"2009":112,"2010":113,"2011":114,"2012":115,"2013":116,"2014":117,"2015":118,"2016":119,"2017":120,"2018":121,"2019":122,"2020":123,"2021":124,"2022":125,"2023":126,"2024":127},{"2009":130,"2010":115,"2011":131,"2012":132,"2013":132,"2014":133,"2015":134,"2016":135,"2017":136,"2018":137,"2019":138,"2020":139,"2021":140,"2022":116,"2023":141,"2024":142},{"2009":145,"2010":146,"2011":147,"2012":148,"2013":149,"2014":150,"2015":151,"2016":152,"2017":153,"2018":154,"2019":155,"2020":156,"2021":157,"2022":158,"2023":159,"2024":100},{"volume":688,"pages":690},{"VOID":689},"34",{"VOID":691},"1732-1743","2023-12-12",2023,{"id":695,"createTime":696,"updateTime":696,"relativeEntities":697,"slug":20,"properties":698,"entityType":181,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21,"primaryUrl":707,"fullTextUrl":20,"authors":708,"publicationType":242,"publisherRelationship":795,"citationCount":20,"citationInfo":20,"publishDate":829,"publishYear":830,"citationAnalyzeStatus":19,"lastCitationAnalyze":20,"indexDatabases":20,"openAccess":20,"references":20,"isForceReanalyzing":546},"12a06fbe-fd95-4396-b56f-1ceb8e9b6abc","2023-12-26T23:54:34.946+00:00",[],{"references":699,"abstract":701,"title":703,"doi":705},{"VOID":700},"Blisniuk, M. P., Hacker, R. B., Glodny, J., et al., 2001. Normal Faulting in Central Tibet since at least 13.5 Ma Ago. Nature, 412: 628–632\nChai, Y. L., Feng, B. G., Yang, J. S., 1984. Features and Origin of Xidatan Granite in Middle East Kunlun Mountains. In: CGQXP Committee, ed., Contribution to Geology of Qinghai-Xizang (Tibet) Plateau (15). Geological Publishing House, Beijing. 79–90 (in Chinese)\nChen, W., Guo, Y. R., Cui, B., et al., 2002. Research on Ages of Deformation and Metamorphism of the Xidatan Rock Series, East Kunlun Mountains. Geological Review, 48(Suppl.): 103–109 (in Chinese with English Abstract)\nCui, J. W., Wu, C. D., Zhu, H., et al., 1996. Deformation and Its Geodynamic Cause of Lithosphere of the Tibetan Plateau. In: Lithosphere Center of CAGS and Institute of Geology of MGMR, ed., Structures, Tectonics and Evolution of Lithosphere of the Tibetan Plateau. Geological Publishing House, Beijing. 58–59 (in Chinese)\nCui, S. Q., Wu, Z. H., 1997. On the Mesozoic and Cenozoic Intracontinental Orogenesis of Yanshan Area, China. Proc. of 30th Int’l. Geol. Congr., 277–292\nCui, Z. Z., 1996. Deep Tectonics and Velocity Structure of Crust-Upper Mantle of the Tibetan Plateau. In: Lithosphere Center of CAGS and Institute of Geology of MGMR, ed., Structures, Tectonics and Evolution of Lithosphere of the Tibetan Plateau. Geological Publishing House, Beijing. 126–137 (in Chinese)\nKidd, W. S. F., Molnar, P., 1990. Quaternary and Present Active Faults of Lhasa-Golmud of the Tibetan Plateau. Roy. Soc. London A, 327: 332–352\nKidd, W. S. F., Pan, Y., Chang, C., et al., 1988. Geological Mapping of the 1985 Chinese-British Tibetan (Xizang- Qinghai) Plateau Geotraverse Route. Phil. Trans. Roy. Soc. London A, 327: 287–305\nLi, J. D., Bai, D. Y., Wang, S. H., 2004. Time of Volcanic Rocks and Peneplanation in Congmeishan Area, North Tibetan Plateau. Geological Bulletin of China, 23(7): 670–675 (in Chinese with English Abstract)\nLi, T. D., 1997. Yadong-Golmud Geoscientific Transection to Show Uplift of the Tibetan Plateau. Earth Science— Journal of China University of Geosciences, 21(1): 34–39 (in Chinese with English Abstract)\nLi, T. D., Xiao, X. C., 1996. Analyses on Terrane Tectonics of the Tibetan Plateau. In: Lithosphere Center of CAGS and Institute of Geology of MGMR, ed., Strutures, Tectonics and Evolution of Lithosphere of the Tibetan Plateau. Geological Publishing House, Beijing. 6–13 (in Chinese)\nLin, A. M., Fu, B. H., Guo, J. M., et al., 2002. Co-seismic Strike-Slip and Rupture Length Produced by the 2001 Ms 8.1 Central Kunlun Earthquake. Science, 296(5575):2015–2017\nPan, G. T., Ding, J., Yao, D. S., et al., 2004. Geological Map of Qinghai-Xizang (Tibet) Plateau and Adjacent Areas (1:1 500 000) Attached with a Guidebook. Chengdu Cartographic Publishing House, Chengdu. 1–48\nPan, Y. S., Kong, X. R., 1998. Lithosphere Structure, Evolution and Dynamics of Qinghai-Xizang (Tibetan) Plateau. Guangdong Science and Technology Press, Guangzhou. 1–428 (in Chinese)\nQinghai Bureau of Geology & Mineral Resources, 1991. Regional Geology of Qinghai Province. Geological Publishing House, Beijing. 1–662 (in Chinese)\nSeismological Bureau of Qinghai Province and Institute of Crust Stress, 1999. East Kunlun Active Fault. Seismological Press, Beijing. 1–186 (in Chinese)\nTapponnier, P., Xu, Z., Roger, F., et al., 2001. Oblique Stepwise Rise and Growth of the Tibet Plateau. Science, 294(5547):1671–1677\nUnsworth, M., Wei, W. B., Alan, G. J., et al., 2004. Crustal and Upper Mantle Structure of Northern Tibet Imaged with Magnetotelluric Data. Journal of Geophysical Research, 109(B2): 1–18\nvan der Woerd, J., Ryerson, F. J., Tapponnier, P., et al., 2000. Uniform Slip-Rate along the Kunlun Fault: Implications for Seismic Behaviour and Large-Scale Tectonics. Geophysical Research Letters, 27(16): 2353–2356\nvan der Woerd, J., Ryerson, F. J., Tapponnier, P., et al., 1998. Holocene Left-Slip Rate Determined by Cosmogenic Surface Dating on the Xidatan Segment of the Kunlun Fault (Qinghai, China). Geology, 26(8): 695–698\nvan der Woerd, J., Tapponnier, P., Ryerson, F. J., et al., 2002. Uniform Postglacial Slip-Rate along the Central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be and 14C Dating of Riser Offsets, and Climatic Origin of the Regional Morphology. Geophysical Journal International, 148(3):356–388\nWang, C. S., Liu, Z. F., Yi, H. S., et al., 2002. Tertiary Crustal Shortening and Peneplanation in the Hoh Xil Region: Implications for Tectonic History of the Northern Tibetan Plateau. Journal of Asian Earth Sciences, 20(3): 211–223\nWei, W., Unsworth, M., Jones, A., et al., 2002. Detection of Widespread Fluids in the Tibetan Crust by Magnetotelluric Studies. Science, 292(5517): 716–718\nWu, Z. H., Barosh, J. P., Wu, Zh. H., et al., 2008. Vast Early Miocene Lakes of the Central Tibetan Plateau. Geological Society of America Bulletin, 120(9–10): 1326–1337\nWu, Z. H., Ye, P. S., Zhao, W. J., et al., 2007. Late Cenozoic Overthrust System in the Southern East Kunlun Mountains, China. Geological Bulletin of China, 26(4): 448–456 (in Chinese with English Abstract)\nWu, Z. H., Hu, D. G., Wu, Z. H., et al., 2006. Pressure Ridges and Their Ages of the Xidatan Strike-Slip Fault in South Kunlun Mts. Geological Review, 52(1): 15–24 (in Chinese with English Abstract)\nWu, Z. H., Hu, D. G., Song, B., et al., 2005. Ages and Thermo-chronological Evolution of the Granite in Northern Xidatan Basin, South Kunlun Mountains Acta Geologica Sinica, 79(5): 628–635 (in Chinese with English Abstract)\nWu, Z. H., Barosh, J. P., Hu, D. G., et al., 2004. Hazards Posed by Active Major Faults along the Golmud-Lhasa Railway Route, Tibetan Plateau, China. Engineering Geology, 74(3–4): 163–182\nXu, Z. Q., Li, H. B., Yang, J. S., et al., 2001. A Large Transpression Zone at the South Margin of the East Kunlun Mountains and Oblique Subduction. Acta Geoscientia Sinica, 75(2): 156–164 (in Chinese with English Abstract)\nYin, A., Harrison, T. M., 2000. Geologic Evolution of the Himalayan- Tibetan Orogen. Annu. Rev. Earth Planet. Sci. Lett., 28: 211–280\nYin, H. F., Zhang, K. X., Wang, G. C., et al., 2003. Regional Geological Report of Donggai Conag Hu Map. China University of Geosciences Press, Wuhan. 282–343 (in Chinese)",{"EN":702},"Southward thrusting occurred in Late Oligocene-Early Miocene in southern East Kunlun (昆仑) Mountains formed the South Kunlun thrust (SKT). Permian strata and Triassic rocks were thrusted over the Paleocene-Eocene red-beds of Fenghuoshan (风火山) Group and Oligocene brownish red conglomerate and sandstone of Yaxicuo (雅西错) Group along SKT faults, formed tectonic slices, low-angle thrust faults, multi-scaled outliers, and nappe structures in south of Middle Kunlun fault (MKF). In addition, SKT displacement or shortening is estimated to be ∼(30–35) km across Dongdatan (东大滩) valley and East Wenquan (温泉) basin. 39Ar-40Ar dating of chlorite of ductile shear zone along front thrust fault indicates that SKT thrusting occurred at 26.5±2.7 Ma, and fission track dating of apatite from mylonitic granite in SKT gives the age 26±2 Ma, corresponding to initial time of rapid uplift of East Kunlun Mountains. Thrust faults and folds of SKT were covered unconformably by Late Miocene lacustrine strata, and major thrusting of SKT ended before 13.5–14.5 Ma according to regional chronological data in northern Tibetan plateau.",{"EN":704},"Late Oligocene-Early Miocene thrusting in southern East Kunlun Mountains, northern Tibetan plateau",{"VOID":706},"10.1007\u002Fs12583-009-0031-2","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12583-009-0031-2",[709,727,739,751,766,778],{"id":710,"sortIndex":711,"researcher":20,"roles":712,"affiliations":713,"properties":724},"028d240d-2270-41fc-9acf-a14849f96a5c",5,[570],[714],{"id":20,"sortIndex":21,"affiliation":715,"properties":20},{"id":716,"createTime":717,"updateTime":718,"relativeEntities":719,"slug":720,"properties":721,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"38292b0d-b985-46a3-816c-4d802cebdafd","2023-12-13T13:37:11.831+00:00","2024-10-12T04:26:43.447+00:00",[],"Institute-of-Geomechanics-Chinese-Academy-of-Geological-Sciences-Beijing-China",{"title":722},{"VI":723},"Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, China",{"title":725},{"VI":726},"Zhonghai Wu",{"id":728,"sortIndex":52,"researcher":20,"roles":729,"affiliations":730,"properties":736},"14380c70-5a6e-475e-9c85-0515d1f69e04",[570],[731],{"id":20,"sortIndex":21,"affiliation":732,"properties":20},{"id":716,"createTime":717,"updateTime":718,"relativeEntities":733,"slug":720,"properties":734,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":735},{"VI":723},{"title":737},{"VI":738},"Daogong Hu",{"id":740,"sortIndex":206,"researcher":20,"roles":741,"affiliations":742,"properties":748},"61d413a4-8633-48a8-afad-99010864c9a3",[570],[743],{"id":20,"sortIndex":21,"affiliation":744,"properties":20},{"id":716,"createTime":717,"updateTime":718,"relativeEntities":745,"slug":720,"properties":746,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":747},{"VI":723},{"title":749},{"VI":750},"Peisheng Ye",{"id":752,"sortIndex":142,"researcher":20,"roles":753,"affiliations":754,"properties":763},"c9eacecd-61b3-4801-aab9-0e575f17cef2",[570],[755],{"id":20,"sortIndex":21,"affiliation":756,"properties":20},{"id":757,"createTime":758,"updateTime":758,"relativeEntities":759,"slug":20,"properties":760,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"7a8cebdd-6199-403e-9fe2-d7b337a2c511","2023-12-26T23:54:34.982+00:00",[],{"title":761},{"VI":762},"P. J. Barosh and Associate, Bristol, USA",{"title":764},{"VI":765},"Barosh J. Patrick",{"id":767,"sortIndex":21,"researcher":20,"roles":768,"affiliations":769,"properties":775},"2e39aa70-13b2-40c8-9510-84f7ccd9cd9d",[570],[770],{"id":20,"sortIndex":21,"affiliation":771,"properties":20},{"id":716,"createTime":717,"updateTime":718,"relativeEntities":772,"slug":720,"properties":773,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":774},{"VI":723},{"title":776},{"VI":777},"Zhenhan Wu",{"id":779,"sortIndex":568,"researcher":20,"roles":780,"affiliations":781,"properties":792},"79c51172-c3f2-4fbb-b243-872a20992031",[570],[782],{"id":20,"sortIndex":21,"affiliation":783,"properties":20},{"id":784,"createTime":785,"updateTime":786,"relativeEntities":787,"slug":788,"properties":789,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"f1977085-b77b-4b20-aaa7-c80059abaed4","2024-02-09T18:15:05.479+00:00","2024-10-16T03:09:04.074+00:00",[],"Chinese-Academy-of-Geological-Sciences-Beijing-China",{"title":790},{"VI":791},"Chinese Academy of Geological Sciences, Beijing, China",{"title":793},{"VI":794},"Wenjin Zhao",{"url":707,"publisher":796,"properties":824},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":797,"slug":10,"properties":798,"entityType":18,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21,"subjectFields":802,"manageAffiliations":803,"indexDatabases":804,"url":93,"thumbnailPath":20,"statistic":819,"gsStatistic":20,"type":160,"analyzePriority":20},[],{"issn":799,"eissn":800,"title":801},{"VOID":13},{"VOID":15},{"EN":17},[],[],[805,812],{"id":75,"indexDatabase":806,"url":88,"indexYears":89,"academicFieldIds":811,"indexDatabaseRanking":92},{"id":77,"createTime":78,"updateTime":79,"relativeEntities":807,"label":808,"description":809,"key":85,"publicationTags":810,"standard":20},[],{"EN":82,"VI":82},{"EN":82,"VI":84},[87],[91],{"id":56,"indexDatabase":813,"url":71,"indexYears":20,"academicFieldIds":818,"indexDatabaseRanking":20},{"id":58,"createTime":59,"updateTime":60,"relativeEntities":814,"label":815,"description":816,"key":67,"publicationTags":817,"standard":20},[],{"EN":63,"VI":63},{"VI":65,"EN":66},[69,70],[73],{"impactFactor":21,"impactFactorByYear":820,"i10Index":108,"i10IndexLast5Year":109,"totalPublication":110,"totalPublicationByYear":821,"totalCitation":128,"totalCitationByYear":822,"totalCitationPerPublication":143,"totalCitationPerPublicationByYear":823,"hindexLast5Year":127,"hindex":127},{"2012":96,"2013":97,"2014":98,"2015":99,"2016":100,"2017":101,"2018":102,"2019":103,"2020":104,"2021":105,"2022":106,"2023":107},{"2009":112,"2010":113,"2011":114,"2012":115,"2013":116,"2014":117,"2015":118,"2016":119,"2017":120,"2018":121,"2019":122,"2020":123,"2021":124,"2022":125,"2023":126,"2024":127},{"2009":130,"2010":115,"2011":131,"2012":132,"2013":132,"2014":133,"2015":134,"2016":135,"2017":136,"2018":137,"2019":138,"2020":139,"2021":140,"2022":116,"2023":141,"2024":142},{"2009":145,"2010":146,"2011":147,"2012":148,"2013":149,"2014":150,"2015":151,"2016":152,"2017":153,"2018":154,"2019":155,"2020":156,"2021":157,"2022":158,"2023":159,"2024":100},{"volume":825,"pages":827},{"VOID":826},"20",{"VOID":828},"381-390","2009-06-07",2009,{"id":832,"createTime":833,"updateTime":833,"relativeEntities":834,"slug":20,"properties":835,"entityType":181,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21,"primaryUrl":844,"fullTextUrl":20,"authors":845,"publicationType":242,"publisherRelationship":911,"citationCount":20,"citationInfo":20,"publishDate":945,"publishYear":946,"citationAnalyzeStatus":19,"lastCitationAnalyze":20,"indexDatabases":20,"openAccess":20,"references":20,"isForceReanalyzing":546},"4944dc7d-525b-42be-bd9a-859eb527b6e7","2023-12-12T23:53:53.981+00:00",[],{"references":836,"abstract":838,"title":840,"doi":842},{"VOID":837},"Chase, Z., Anderson, R. F., Fleisher, M. Q., 2001. Evidence from Authigenic Uranium for Increased Productivity of the Glacia Subantarctic Ocean. Paleoceanography, 16: 468–478\nChen, J. F., Zhang, Y. C., Sun, S. L., et al., 2006. Main Factors Influencing Marine Carbonate Source Rock Formation. Acta Geologica Sinica, 80(3): 467–472 (in Chinese with English Abstract)\nDeng, H. W., Qian, K., 1993. Sedimentary Geochemistry and Environmental Analysis. Gansu Science and Technology Publishing House, Lanzhou. 1–82 (in Chinese)\nGao, J. P., 2008. The Tectonic Characteristics and Petroleum Geological Conditions of Foreland Thrust Belt in the Eastern Section of the Southern Junggar Basin: [Dissertation]. Northwest University, Xi’an. 12–46 (in Chinese with English Abstract)\nHatch, J. R., Leventhal, J. S., 1992. Relationship between Inferred Redox Potential of the Depositional Environment and Geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limstone, Wabaunsee Countr, Kansas, U.S.A.. Chemical Geology, 99: 65–82\nHu, X. F., Liu, Z. J., Liu, R., et al., 2012a. Clay Mineral and Inorganic Geochemical Characteristics of Eocene Huadian Formation in Huadian Basin and Their Paleoenvironment Implications. Journal of China Coal Society, 37(3): 416–423 (in Chinese with English Abstract)\nHu, X. F., Liu, Z. J., Liu, R., et al., 2012b. Trace Element Characteristics of Eocence Jijuntun Formation and the Favorable Metallogenic Conditions of Oil Shale in Fushun Basin. Journal of Jilin University (Earth Science Edition), 42(Suppl.): 60–71 (in Chinese with English Abstract)\nJin, B. F., Lin, Z. H., Yang, Q. H., et al., 2002. Application of Sedimentary Mineralogy to the Environmental Analysis in Marginal Seas. Marine Geology & Quater nary Geology, 22(3): 113–117 (in Chinese with English Abstract)\nJones, B. J., Manning, A. C., 1994. Comparison of Geochemical Indices Used for the Interpretation of Palaeoredox Conditions in Ancient Mudstones. Chemical Geology, 11(11): 111–129\nKuang, L. X., Guo, J. H., Tong, X. L., et al., 2007. Forming Conditions and Patterns of Hydrocarbon Reservoirs in East of Southern Fringe of Junggar Basin. Earth Sciences and Environment, 29(1): 34–40 (in Chinese with English Abstract)\nLan, X. H., Ma, D. X., Xu, M. G., et al., 1987. Some Geochemical Signs and Their Importance for Sedimentary Facies. Marine Geology and Quaternary Geology, 7(1): 39 (in Chinese with English Abstract)\nLi, C. B., Guo, W., Song, Y. Q., et al., 2006. The Genetic Type of the Oil Shale at the Northern Foot of Bogeda Mountain, Xinjiang and Prediction for Favorable Areas. Journal of Jilin University (Earth Science Edition), 36(6): 949–953 (in Chinese with English Abstract)\nLi, J. J., 2009. Study on the Oil Shale Geochemistry of Permian Lucaogou Formation in the Northern Bogda Moutain: [Dissertation]. China University of Geosciences, Beijing. 1–90 (in Chinese with English Abstract)\nLi, N., Hu, C. Y., Ma, Z. W., 2011. Main Control Factors of High Quality Hydrocarbon Source Rocks of the Upper Permian Dalong Formation at Shangsi Section of Guangyuan, Sichuan Province. Palaeogeography, 13(3): 347–353 (in Chinese with English Abstract)\nLi, S. J., Xiao, K. H., Wo, Y. J., et al., 2008. REE Geochemical Characteristics and Their Geological Signification in Silurian, West of Hunan Province and North of Guizhou Province. Geoscience, 22(2): 273–280 (in Chinese with English Abstract)\nLyons, T. W., Werne, J. P., Holander, D. J., et al., 2003. Contrasting Sulfer Geochemistry and Fe\u002FAl And Mo\u002FAl Ratios across the Last Oxic-Anoxic Transition in the Cariaco Basin, Venezuela. Chemical Geology, 195: 131–157\nPeng, X. F., Wang, J. L., Jiang, L. P., 2012. Geochemical Characteristics of the Lucaogou Formation Oil Shale in the Southeastern Margin of the Junggar Basin and Its Environmental Implications. Bulletin of Mineralogy, Petrology and Geochemistry, 31(2): 121–157 (in Chinese with English Abstract)\nQin, J. Z., Liu, B. Q., Guo, S. Z., et al., 2005. China Hydrocarbon Source Rocks. Science Publishing House, Beijing. 1–163 (in Chinese)\nTenger, Liu, W. H., Xu, Y. C., 2006. Comprehensive Geochemical Identification of Highly Evolved Marine Hydrocarbon Source Rocks: Organic Matter, Paleoenvironment and Development of Effective Hydrocarbon Source Rocks. Chinese Journal of Geochemistry, 25(4): 332–339\nWang, C. L., Liu, C. L., Hu, H. B., et al., 2012. Sedimentary Characteristics and Its Environmental Significance of Salt-Bearing Strata of the Member 4 of Paleocene Shashi Formation in Southern Margin of Jiangling Depression, Jianghan Basin. Palaeogeography, 14(2): 165–175 (in Chinese with English Abstract)\nWang, S. B., Sun, Y., Zhong, J. H., et al., 2008. The Influence of the Ancient Climate Changes on the Development of Sequence Development in the Late Cretaceous in Songliao Basin. Petroleum Geology and Engineering, 22(4): 29–32 (in Chinese)\nWang, X. W., Wang, X. W., Ma, Y. S., et al., 2007. The Tectonic Evolution of Bogda Mountain, Xinjiang Northwest China and Its Relationship to Oil and Gas Accumulation. Geoscience, 21(1): 116–124 (in Chinese with English Abstract)\nWang, Z. M., 2003. Geochemical Indicators Fordiagnosing Anoxic Sedimentary Environment. Acta Geologica Gansu, 12(2): 55–58 (in Chinese with English Abstract)\nWilde, P., Quinby, M. S., Lyons, T. W., 2001. Molybdenum as an Indicator of Original Organic Content in Ancient Anoxic Sediments. Geological Society of American, 33(6): 39 (Abstracts with Programs)\nZhang, M. M., Liu, Z. J., Xu, S. C., et al., in press. Analysis for the Paleosalinity and Lake-Level Changes of the Oil Shale Measures in the Lucaogou Formation in Sangonghe Area of Southern Margin, Junggar Basin. Petroleum Science and Technology",{"EN":839},"With the analysis of the element geochemistry characteristics, the ancient lake information evolution history of the argillaceous source rocks in Lucaogou (芦草沟) Formation in Sangonghe (三工河) area is reconstructed. According to the ancient lake information and total organic matter (TOC) characteristics of argillaceous source rocks, the study section is divided into 6 Subsections. Subsection I mainly developed low-quality source rocks. This is because of the arid climate, high salinity, low lake productivity, unstable preservation conditions in this Subsection. Subsection II mainly developed high-quality source rocks. This is because of the humid climate, low salinity, high lake productivity, stable preservation conditions in this Subsection. Though the paleoclimate was humid and preservation conditions were stable. Lake productivity and the water salinity changed frequently. So Subsection III mainly developed medium-quality source rocks. Because of the humid climate, high lake productivity, medium sedimentary rate and stable preservation conditions, high-quality source rocks were developed in Subsection IV. The preservation conditions were stable, but other ancient lake information changed frequently. Therefore, the quality of the formed source rocks in Subsection V was different. Subsection VI mainly developed high-quality source rocks because of the humid climate, medium sedimentary rate, high lake productivity, low salinity and good preservation conditions. In summary, the ancient lake information parameters and TOC characteristics of each Subsection are different from each other.",{"EN":841},"Element response to the ancient lake information and its evolution history of argillaceous source rocks in the Lucaogou Formation in Sangonghe area of southern margin of Junggar Basin",{"VOID":843},"10.1007\u002Fs12583-013-0392-4","http:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs12583-013-0392-4",[846,863,875,887,899],{"id":847,"sortIndex":142,"researcher":20,"roles":848,"affiliations":849,"properties":860},"ba50959d-08db-41fa-956d-747f1cf77702",[570],[850],{"id":20,"sortIndex":21,"affiliation":851,"properties":20},{"id":852,"createTime":853,"updateTime":854,"relativeEntities":855,"slug":856,"properties":857,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"92650597-3efc-4b9c-97f2-9a7caa35b3ec","2024-01-15T18:14:58.999+00:00","2024-11-28T04:32:19.364+00:00",[],"College-of-Earth-Sciences-Jilin-University-Changchun-China",{"title":858},{"VI":859},"College of Earth Sciences, Jilin University, Changchun, China",{"title":861},{"VI":862},"Shengchuan Xu",{"id":864,"sortIndex":568,"researcher":20,"roles":865,"affiliations":866,"properties":872},"984c2719-f3bd-4c3c-b414-f335fee29916",[570],[867],{"id":20,"sortIndex":21,"affiliation":868,"properties":20},{"id":852,"createTime":853,"updateTime":854,"relativeEntities":869,"slug":856,"properties":870,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":871},{"VI":859},{"title":873},{"VI":874},"Xiaofeng Hu",{"id":876,"sortIndex":21,"researcher":20,"roles":877,"affiliations":878,"properties":884},"4b0a7469-bdbd-4c52-94eb-92158c7409eb",[570],[879],{"id":20,"sortIndex":21,"affiliation":880,"properties":20},{"id":852,"createTime":853,"updateTime":854,"relativeEntities":881,"slug":856,"properties":882,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":883},{"VI":859},{"title":885},{"VI":886},"Mingming 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P. A., Allen, J. R., 2005. Basin Analysis: Principle and Applications. Blackwell, Oxford. 1–493\nCatuneanu, O., Abreu, V., Bhattacharya, J. P., et al., 2009. Towards the Standardization of Sequence Stratigraphy. Earth-Science Reviews, 92(1\u002F2): 1–33. doi:10.1016\u002Fj.earscirev.2008.10.003\nDeng, H. W., Guo, J. Y., Wang, R. J., et al., 2008. Tectono-Sequence Stratigraphic Analysis in Continental Faulted Basins. Earth Science Frontier, 15(2): 1–7 (in Chinese with English Abstract)\nFeng, Y. L., Xu, X. S., 2006. Syndepositional Structural Slope-Break Zone Controls on Lithologic Reservoirs-A Case from Paleogene Bohai Bay Basin. Petroleum Exploration and Development, 33(1): 22–31 (in Chinese with English Abstract)\nFeng, Y. L., Zhou, H. M., Ren, J. Y., et al., 2010. Paleogene Sequence Stratigraphy in the East of the Bohai Bay Basin and Its Response to Structural Movement. Sci. Sin. Terrae, 40(10): 1356–1376 (in Chinese with English Abstract)\nHaq, B. U., Hardenbol, J., Vail, P. R., 1987. Chronology of Fluctuating Sea Levels since the Triassic. Science, 235(4793): 1156–1167. doi:10.1126\u002Fscience.235.4793.1156\nHuang, C. Y., Wang, H., Wu, Y. P., et al., 2012. Genetic Types and Sequence Stratigraphy Models of Palaeogene Slope Break Belts in Qikou Sag, Huanghua Depression, Bohai Bay Basin, Eastern China. Sedimentary Geology, 261\u002F262: 65–75. doi:10.1016\u002Fj.sedgeo.2012.03.005\nHou, Y. G., He, S., Ni, J. E., et al., 2012. Tectono-Sequence Stratigraphic Analysis on Paleogene Shahejie Formation in the Banqiao Sub-Basin, Eastern China. Marine and Petroleum Geology, 36(1): 100–117. doi:10.1016\u002Fj.marpetgeo.2012.06.001\nLei, C., Ren, J. Y., Li, X. S., et al., 2011. Structural Characteristics and Petroleum Exploration Potential in the Deep-Water Area of the Qiongdongnan Basin, South China Sea. Petroleum Exploration and Development, 38(5): 560–569 (in Chinese with English Abstract)\nLi, S. T., Lin, C. S., Zhang, Q. M., et al., 1999. Episodic Rifting of Continental Marginal Basins and Tectonic Events since 10 Ma in the South China Sea. Chinese Science Bulletin, 44(1): 10–23. doi:10.1007\u002Fbf03182877\nLi, S. T., Pan, Y. L., Lu, Y. C., et al., 2002. Key Technology of Prospecting and Exploration of Subtle Traps in Lacustrine Fault Basins: Sequence Stratigraphic Researches on the Basis of High Resolution Seismic Survey. Earth Science-Journal of China University of Geosciences, 27: 592–598 (in Chinese with English Abstract)\nLi, S. T., Xie, X. N., Wang, H., et al., 2004. Sedimentary Basin Analysis Principle and Application. Higher Education Press, Beijing. 1–410 (in Chinese)\nLiao, J. H., Wang, H., Sun, Z. P., et al., 2012. Tectonic Evolution and Its Controlling on Sequence Pattern of Chang-Chang Sag, Deepwater Area of Qiongdongnan Basin, South China Sea. Journal of Central South University (Science and Technology), 43: 3121–3132 (in Chinese with English Abstract)\nLin, C. S., 2009. Sequence and Depositional Architecture of Sedimentary Basin and Process Responses. Acta Sedimentologica Sinica, 27: 849–862 (in Chinese with English Abstract)\nLin, C. S., Kenneth, E., Li, S. T., et al., 2001. Sequence Architecture, Depositional Systems, and Controls on Development of Lacustrine Basin Fills in Part of the Earlian Basin, Northeast China. AAPG Bulletin, 85(11): 2017–2043\nLin, C. S., Zhang, Y. M., Li, S. T., et al., 2004. Episodic Rifting Dynamic Process and Quantitative Model of Mesozoic–Cenozoic Faulted Basins in Eastern China. Earth Science-Journal of China University of Geosciences, 29(5): 583–588 (in Chinese with English Abstract)\nLiu, E. T., Wang, H., Lin, Z. L., et al., 2012. Characteristics and Hydrocarbon Enrichment Rules of Transfer Zone in Fushan Sag, Beibuwan Basin. Journal of Central South University (Science and Technology), 43: 3946–3953 (in Chinese with English Abstract)\nLiu, E. T., Wang, H., Li, Y., et al., 2014. Sedimentary Characteristics and Tectonic Setting of Sublacustrine Fans in a Half-Graben Rift Depression, Beibuwan Basin, South China Sea. Marine and Petroleum Geology, 52: 9–21. doi:10.1016\u002Fj.marpetgeo.2014.01.008\nLiu, H., Wang, Y. M., Xin, R. C., et al., 2006. Study on the Slope Break Belts in the Jurassic Down-Warped Lacustrine Basin in Western-Margin Area, Junggar Basin, Northwestern China. Marine and Petroleum Geology, 23(9\u002F10): 913–930. doi:10.1016\u002Fj.marpetgeo.2006.08.004\nLiu, L. J., Kuang, H. W., Tong, Y. M., et al., 2003. Sedimentary Systems and Evolution Characteristics of Lower Tertiary Liushagang Formation in Fushan Sag. Oil & Gas Geology, 24(2): 140–145 (in Chinese with English Abstract)\nMa, Q. L., Zhao, S. E., Liao, Y. T., et al., 2012. Sequence Architectures of Paleogene Liushagang Formation and Its Significance in Fushan Sag of the Reibuwan Basin. Earth Science-Journal of China University of Geosciences, 37(4): 667–678 (in Chinese with English Abstract)\nMa, Y., Li, S. Z., Zhang, B. K., et al., 2013. Unconformities in the Beibuwan Basin and Their Implications for Tectonic Evolution. Marine Geology & Quaternary Geology, 33(2): 63–72 (in Chinese with English Abstract)\nRen, J. Y., Lu, Y. C., Zhang, Q. L., et al., 2004. Forming Mechanism of Structural Slope-Break and Its Control on Sequence Style in Faulted Basin. Earth Science-Journal of China University of Geosciences, 29(5): 596–602 (in Chinese with English Abstract)\nShi, Y. M., Liu, J., Zhang, M. Z., et al., 2007. Experience and Understand in Oil and Gas Exploration in Fushan Sag, Hainan Province. South China Journal of Selsmology, 27(3): 57–68 (in Chinese with English Abstract)\nSong, G. Z., Wang, H., Gan, H. J., et al., 2014. Paleogene Tectonic Evolution Controls on Sequence Stratigraphic Patterns in the Central Part of Deepwater Area of Qiongdongnan Basin, Northern South China Sea. Journal of Earth Science, 25(2): 275–288. doi:10.1007\u002Fs12583-014-0433-7\nVan Wagoner, J. C., Mitchum, R. M., Campion, K., et al., 1990. Siliciclastic Sequence Stratigraphy in Well Logs, Cores and Outcrops: Concepts for High Resolution Correlation of Time and Facies. AAPG Methods in Exploration Series, 7: 1–55\nVail, P. R., Mitchum, R. M., Thompson, S., 1977. Global Cycles of Relative Changes of Sea Level. AAPG Bulletin, 26: 99–116\nWang, G. H., Huang, C. Y., Liu, E. T., et al., 2014. Characteristics of Slope-Breaks and Its Control on Sedimentation and Hydrocarbon Accumulation of Liushagang Formation in Gentle Slope, South Fushan Sag. Journal of Central South University (Science and Technology), 45(5): 1–11 (in Chinese with English Abstract)\nXie, X. N., Müller, R. D., Ren, J. Y., et al., 2008. Stratigraphic Architecture and Evolution of the Continental Slope System in Offshore Hainan, Northern South China Sea. Marine Geology, 247(3\u002F4): 129–144. doi:10.1016\u002Fj.margeo.2007.08.005\nXu, H., 1997. Some Problems in Study of Continental Sequence Stratigraphy. Oil & Gas Geology, 18: 83–89 (in Chinese with English Abstract)\nXu, J. Y., Zhang, G. C., Liang, J. S., et al., 2011. Paleogene Activities of Episode Rifting and Their Relationships with Hydrocarbon in Beibuwan Basin. China Offshore Oil and Gas, 23(6): 362–368 (in Chinese with English Abstract)\nZhang, Z. W., Liu, Z. F., Zhang, G. C., et al., 2013. The Chasmic Stage and Structural Evolution Features of Beibuwan Basin. Journal of Oil and Gas Technology, 35(1): 6–10 (in Chinese with English Abstract)",{"EN":955},"Tectonism is of extreme importance to sequence stratigraphic patterns in continental sedimentary basins, affecting both the architectures and internal makeup of sequences. Sequence stratigraphic framework of the Paleogene system in the Fushan sag, northern South China Sea, was built using 3D and 2D seismic data, complemented by drilling cores and well logs data. One first-order, three second-order and seven third-order sequences were identified. Analysis of paleotectonic stress field, unconformities and subsidence history showed that the Paleogene tectonic evolution presented significant characteristics of multistage and episode, and can be divided into three stages: rifting stage I (initial rifting period), rifting stage II (rapid subsidence period), rifting stage III (fault-depressed diversionary period). Partition of the west and east in tectonic activity was obvious. The west area showed relatively stronger tectonic activity than the east area, especially during the rifting stage II. Episodic rifting and lateral variations in tectonic activity resulted in a wide variety of structural slope break belts, which controlled both the sequence architectures and interval makeup, and strongly constrained the development of special facies zones or sand bodies that tended to form hydrocarbon accumulation. This paper classifies the genetic types of slope break belts and their relevant sequence stratigraphic patterns within the Fushan sag, and further discusses the tectonic evolution controls on sequence stratigraphic patterns, which suggests that vertical evolution paths of structural slope break belts and relevant sequence stratigraphic patterns as a response to the Paleogene tectonic evolution were strongly controlled by sag margin types and lateral variations of tectonic activity.",{"EN":957},"Paleogene tectonic evolution controls on sequence stratigraphic patterns in the Fushan sag, northern South China 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W. Y., Li, Y. H., 1994. The Determination of U and Th by the Extraction-Liqiud Scintillation-α Spectrum Analysis Method. Nuclear Techniques, 1: 47–50 (in Chinese with English Abstract)\nKang, T. S., Wang, S. C., 1991. Fission Track Method for the Research of Geological Thermal History. Science Press, Beijing. 14–15 (in Chinese)\nLu, X. T., 2000. Nuclear Physics. The Atom Publishing House, Beijing. 10, 38 (in Chinese)\nWang, X. L., 1991. Application of a New Reagent to Determining Microthorium Contentinrocks. Scientia Geologica Sinica, 3: 299–302 (in Chinese with English Abstract)\nYang, T. S., 2007. Thermal Analysis Detection Solid Nuclear Path to the Feasibility Study of Trace. Chinese Science Bulletin, 52(2): 380–383 (in Chinese)\nYang, T. S., He, S. R., Li, T. X., et al., 2009. Measurement of Solid State Nuclear Tracks in Apatite by Thermal Analysis Method. Chinese Science Bulletin, 54(17): 2495–2499 (in Chinese)",{"EN":1132},"On the basis of previous research achievements of measuring the solid state nuclear track in apatite by thermal analysis method, the author further proposes the research program to measure the energy deposited by the solid state nuclear track contained in zircon, sphene, epidote, apatite and other samples, in order to study the geological age and geothermal history. Compared with the measurement of nuclear track density by etching method, this one does not need to conduct so many processing programs for samples, but can improve the measurement accuracy.",{"EN":1134},"Research program of determination of geological age by thermal analysis 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W., 1988. Interpratation of the Positive-Degree-Days Factor by Heat Balance Characteristics, West Greenland. Nordic Hydrology, 19: 217–224\nArnold, N. S., Willis, I. C., Sharp, M. J., et al., 1996. A Distributed Surface Energy-Balance Model for a Small Valley Glacier. I. Development and Testing for Haut Glacier d’Arolla, Valais, Switzerland. Journal of Glaciology, 42(140): 77–89\nBai, Z. Y., 1989. A Study of Relationship between Climate and Mountain Glaciers. Journal of Glaciology and Geocryology, 11(4): 287–297 (in Chinese with English Abstract)\nBamber, J. L., Payne, A. J., 2004. Mass Balance of the Cryosphere: Observations and Modelling of Contemporary and Future Changes. Cambridge University Press, Cambridge\nBlöschl, G., Kirnbauer, R., Gutknecht, D., 1991. Distributed Snowmelt Simulations in an Alpine Catchment I: Model Evaluation on the Basis of Snow Cover Patterns. Water Resource Research, 27(12): 3171–3179\nBraithwaite, R. J., 1995. Positive Degree Day Factors for Ablation on the Greenland Ice Sheet Studied by Energy: Balance Modeling. Journal of Glaciology, 41(137): 153–160\nBraithwaite, R. J., Konzelmann, T., Marty, C., et al., 1998. Errors in Daily Ablation Measurements in Northern Greenland, 1993–94, and Their Implications for Glacier Climate Studies. Journal of Glaciology, 44(148): 583–588\nBraithwaite, R. J., Olesen, O. B., 1989. Criminological Theory and Organizational Crime. Justice Quarterly, 6: 333–358\nBraithwaite, R. J., Zhang, Y., 2000. Sensitivity of Mass Balance of Five Swiss Glaciers to Temperature Changes Assessed by Tuning a Degree-Day Model. Journal of Glaciology, 46(152): 7–14\nCui, Y. H., 2009. Analysis of Spatial and Temporal Variation about Degree-Day Factor at Glacier No. 1 at the Headwaters of the Urumchi River: [Dissertation]. Graduate University of Chinese Academy of Sciences, Beijing (in Chinese with English Abstract)\nFinsterwalder, S., Schunk, H., 1887. Der Suldenferner. Zeitschrift des Deutschen und Oesterreichischen Alpenvereins, 18: 72–89 (in German)\nHe, Y, Q., Yao, T. D., Yang, M. X., 2000. Spatial Features of Glacial Hydro-chemistry and Recent Variations of a Chinese Temperate Glacier in Mt. Yulong. Journal of Mountain Science, 6(18): 481–488 (in Chinese with English Abstract)\nHe, Y. Q., Yao, T. D., Theakstone, W. H., 1999. Analysis of Climatic and Environmental Records in an Alpine Temperate Glacier. Journal of Glaciology and Geocryology, 21(3): 257–263 (in Chinese with English Abstract)\nHe, Y. Q., Zhang, D., 2004. Climatic Warming is the Major Reason for Glacier Retreat on Mt. Yulong, China. Journal of Glaciology and Geocryology, 26(2): 230–231 (in Chinese)\nHock, R., 1999. A Distributed Temperature-Index Ice and Snowmelt Model Including Potential Direct Solar Radiation. Journal of Glaciology, 45(149): 101–111\nHock, R., 2003. Temperature Index Melt Modeling in Mountain Areas. Journal of Hydrology, 282(1–4): 104–115\nHock, R., 2005. Glacier Melt: A Review on Processes and Their Modeling. Progress in Physical Geography, 29(3): 362–391\nKang, E. S., Liu, C. H., 1994. A Characteristics Mass Balance of Glacier No. 1 at the Headwaters of the Urumuqi River. Advance in Earth Sciences, 16(2): 119–127\nKayastha, R. B., Ageta, Y., Nakawo, M., et al., 2003. Positive Degree-Day Factors for Ice Ablation on Four Glaciers in the Nepalese Himalayas and Qinghai-Tibetan Plateau. Bulletin of Glaciological Research, 20: 7–14\nKustas, W. P., Rango, A., Uijlenhoet, R., 1994. A Simple Energy Budget Algorithm for the Snowmelt Runoff Model. Water Resources Research, 30(5): 1515–1527\nLaumann, T., Reeh, N., 1993. Sensitivity to Climate Change of the Mass Balance of Glaciers in Southern Norway. Journal of Glaciology, 39(133): 656–665\nLi, J. J., 1996. Glaciers in the Hengduan Mountains. Science Press, Beijing (in Chinese)\nLiu, S. Y., Ding, Y. J., Wang, N. L., et al., 1998. Mass Balance Sensitivity to Climate Change of the Glacier No. 1 at the Urumqi River Head, Tianshan Mts.. Journal of Glaciology and Geocryology, 20(1): 9–13 (in Chinese with English Abstract)\nShi, Y. F., 2005, China Glacier Inventory (CGI). Shanghai Science Popularization, Shanghai (in Chinese)\nSong, B., 2008, Application Study in China’s Monsoonal Temperate-Glacier Regions Based on GIS and Remote Sensing: [Dissertation]. Graduate University of Chinese Academy of Sciences, Beijing (in Chinese with English Abstract)\nWorld Meteorological Organization (WMO), 1986. Intercomparison of Models of Snowmelt Runoff. Operational Hydrological Report No. 23. Geneva, Switzerland\nYang, Z. N., Liu, X. N., Zeng, Q. Z., 2000. Arid Region Hydrology in China. Science Press, Beijing. 35–54 (in Chinese)\nZhang, Y., Liu, S. Y., Ding, Y. J., 2006. Spatial Variation of Degree-Day Factors on the Observed Glaciers in Western China. Acta Geographica Sinica, 61(1): 89–98 (in Chinese with English Abstract)\nZhang, Y., Liu, S. Y., Shangguan, D. H., et al., 2005. Study of the Positive Degree-Day Factors on the Koxkar Baqi Glacier on the South Slope of Tianshan Mountains. Journal of Glaciology and Geocryology, 27(3): 337–343 (in Chinese with English Abstract)\nZhao, X. T., Qu, Y. X., Li, T. S., 1999. Pleistocene Glaciations along the Eastern Foot of the Yulong Mountains. Journal of Glaciology and Geocryology, 21(3): 242–248 (in Chinese with English Abstract)\nZheng, B. X., 2000. Quaternary Glaciation and Glacier Evolution in the Yulong Mount, Yunnan. 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Marees Terr., 124: 9425–9439",{"EN":1446},"Using 1 Hz sampling records at one superconducting gravimeter (SG) station and 11 broadband seismometer stations, we found anomalous signals prior to the 2008 Wenchuan (汶川) earthquake event. The tides are removed from the original SG records to obtain the gravity residuals. Applying the Hilbert-Huang transform (HHT) and the wavelet analysis to the SG gravity residuals leads to time-frequency spectra, which suggests that there is an anomalous signal series around 39 h prior to the event. The period and the magnitude of the anomalous signal series are about 8 s and 3×10−8 m\u002Fs2 (3 μGal), respectively. In another aspect, applying HHT analysis technique to 11 records at broadband seismometer stations shows that most of them contain anomalous signals prior to the Wenchuan event, and the marginal spectra of 8 inland stations show an apparent characteristic of double peaks in anomalous days compared to the only one peak of the marginal spectra in quiet days. Preliminary investigations suggest that the anomalous signals prior to the earthquake are closely related to the low-frequency earthquake (LFE). We concluded that the SG data as well as the broadband seismometers records might be significant information sources in detecting the anomalous signals prior to large earthquakes.",{"EN":1448},"Anomalous signals prior to Wenchuan earthquake detected by superconducting gravimeter and broadband seismometers records",{"VOID":1450},"10.1007\u002Fs12583-011-0215-4","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12583-011-0215-4",[1453,1468,1493],{"id":1454,"sortIndex":142,"researcher":20,"roles":1455,"affiliations":1456,"properties":1465},"79831145-f882-4e60-9c76-7d223cfb0a44",[570],[1457],{"id":20,"sortIndex":21,"affiliation":1458,"properties":20},{"id":1459,"createTime":1460,"updateTime":1460,"relativeEntities":1461,"slug":20,"properties":1462,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"acc146d5-24c8-4613-9422-2d800de07b10","2023-12-28T03:04:34.635+00:00",[],{"title":1463},{"VI":1464},"Department of Civil Engineering, National Chiao Tung University, Taipei, China",{"title":1466},{"VI":1467},"Cheinway Hwang",{"id":1469,"sortIndex":21,"researcher":20,"roles":1470,"affiliations":1471,"properties":1490},"7adcbdaf-8292-459b-adfa-035cb7937fb5",[570],[1472,1482],{"id":1473,"sortIndex":206,"affiliation":1474,"properties":1481},"8635102b-a432-4964-b231-b410d1f213ea",{"id":1475,"createTime":1476,"updateTime":1476,"relativeEntities":1477,"slug":20,"properties":1478,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"554123ae-9ccd-4936-ad01-71e5ee3ecd18","2024-01-14T12:10:52.664+00:00",[],{"title":1479},{"VI":1480},"Key Laboratory of Geospace Environment and geodesy, Wuhan University, Wuhan, China",{},{"id":20,"sortIndex":21,"affiliation":1483,"properties":20},{"id":1484,"createTime":1485,"updateTime":1485,"relativeEntities":1486,"slug":20,"properties":1487,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"9135b9ce-7121-49cb-814f-1812887ac117","2024-02-10T09:57:24.484+00:00",[],{"title":1488},{"VI":1489},"Department of Geophysics, School of Geodesy and Geomatics, Wuhan University, Wuhan, China",{"title":1491},{"VI":1492},"Wenbin 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A Mixed Seawater and Hydrothermal Origin of Superior-Type Banded Iron Formation (BIF)-Hosted Kouambo Iron Deposit, Palaeoproterozoic Nyong Series, Southwestern Cameroon: Constraints from Petrography and Geochemistry. Ore Geology Reviews, 80: 860–875. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2016.08.021\nGurvich, E. G., 2006. Metalliferous Sediments of the World Ocean: Fundamental Theory of Deep-Sea Hydrothermal Sedimentation. Springer, Berlin\nHagemann, S. G., Angerer, T., Duuring, P., et al., 2016. BIF-Hosted Iron Mineral System: A Review. Ore Geology Reviews, 76: 317–359. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2015.11.004\nHensler, A. S., Hagemann, S. G., Rosière, C. A., et al., 2015. Hydrothermal and Metamorphic Fluid-Rock Interaction Associated with Hypogene “Hard” Iron Ore Mineralisation in the Quadrilátero Ferrífero, Brazil: Implications from in-situ Laser Ablation ICP-MS Iron Oxide Chemistry. Ore Geology Reviews, 69: 325–351. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2015.02.023\nHouketchang Bouyo, M., Penaye, J., Mouri, H., et al., 2019. Eclogite Facies Metabasites from the Paleoproterozoic Nyong Group, SW Cameroon: Mineralogical Evidence and Implications for a High-Pressure Metamorphism Related to a Subduction Zone at the NW Margin of the Archean Congo Craton. Journal of African Earth Sciences, 149: 215–234. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jafrearsci.2018.08.010\nHu, H., Lentz, D., Li, J. W., et al., 2014. Re-Equilibration Processes of Magnetite from Iron Skarn Deposits. Acta Geologica Sinica: English Edition, 88(s2): 354–356. https:\u002F\u002Fdoi.org\u002F10.1111\u002F1755-6724.12372_4\nHu, H., Li, J. W., Harlov, D. E., et al., 2020. A Genetic Link between Iron Oxide-Apatite and Iron Skarn Mineralization in the Jinniu Volcanic Basin, Daye District, Eastern China: Evidence from Magnetite Geochemistry and Multi-Mineral U-Pb Geochronology. GSA Bulletin, 132(5\u002F6): 899–917. https:\u002F\u002Fdoi.org\u002F10.1130\u002Fb35180.1\nKnipping, J. L., Bilenker, L. D., Simon, A. C., et al., 2015. Trace Elements in Magnetite from Massive Iron Oxide-Apatite Deposits Indicate a Combined Formation by Igneous and Magmatic-Hydrothermal Processes. Geochimica et Cosmochimica Acta, 171: 15–38. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.gca.2015.08.010\nKwamou, W. M. M., Djibril, K. N. G., Guimollaire, N. D., et al., 2021. Petrogenesis and U-Pb Zircon Dating of Amphibolite in the Mewengo Iron Deposit, Nyong Series, Cameroon: Fingerprints of Iron Depositional Geotectonic Setting. Arabian Journal of Geosciences, 14(10): 872. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12517-021-07235-8\nLerouge, C., Cocherie, A., Toteu, S. F., et al., 2006. Shrimp U-Pb Zircon Age Evidence for Paleoproterozoic Sedimentation and 2.05 Ga Syntectonic Plutonism in the Nyong Group, South-Western Cameroon: Consequences for the Eburnean-Transamazonian Belt of NE Brazil and Central Africa. Journal of African Earth Sciences, 44(4\u002F5): 413–27. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jafrearsci.2005.11.010\nLi, H. M., Zhang, Z. J., Li, L. X., et al., 2014. Types and General Characteristics of the BIF-Related Iron Deposits in China. Ore Geology Reviews, 57: 264–287. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2013.09.014\nLi, Y. L., Konhauser, K. O., Zhai, M. G., 2017. The Formation of Magnetite in the Early Archean Oceans. Earth and Planetary Science Letters, 466: 103–114. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.epsl.2017.03.013\nLiu, L., Zhang, H. S., Yang, X. Y., et al., 2018. Age, Origin and Significance of the Wugang BIF in the Taihua Complex, Southern North China Craton. Ore Geology Reviews, 95: 880–898. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2018.04.005\nLiu, L., Zhang, L. C., Dai, Y. P., 2014. Formation Age and Genesis of the Banded Iron Formations from the Guyang Greenstone Belt, Western North China Craton. Ore Geology Reviews, 63: 388–404. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2013.10.011\nLiu, Y. S., Hu, Z. C., Gao, S., et al., 2008. In situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1\u002F2): 34–43. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.chemgeo.2008.08.004\nLoose, D., Schenk, V., 2018. 2.09 Ga Old Eclogites in the Eburnian-Transamazonian Orogen of Southern Cameroon: Significance for Palaeoproterozoic Plate Tectonics. Precambrian Research, 304: 1–11. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.precamres.2017.10.018\nManikyamba, C., Balaram, V., Naqvi, S. M., 1993. Geochemical Signatures of Polygenetic Origin of a Banded Iron Formation (BIF) of the Archaean Sandur Greenstone Belt (Schist Belt) Karnataka Nucleus, India. Precambrian Research, 61(1\u002F2): 137–164. https:\u002F\u002Fdoi.org\u002F10.1016\u002F0301-9268(93)90061-6\nMoudioh, C., Soh Tamehe, L., Ganno, S., et al., 2020. Tectonic Setting of the Bipindi Greenstone Belt, Northwest Congo Craton, Cameroon: Implications on BIF Deposition. Journal of African Earth Sciences, 171: 103971. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jafrearsci.2020.103971\nNadoll, P., Angerer, T., Mauk, J. L., et al., 2014. The Chemistry of Hydrothermal Magnetite: A Review. Ore Geology Reviews, 61: 132. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2013.12.013\nNdime, E. N., Ganno, S., Nzenti, J. P., 2019. Geochemistry and Pb-Pb Geochronology of the Neoarchean Nkout West Metamorphosed Banded Iron Formation, Southern Cameroon. International Journal of Earth Sciences, 108(5): 1551–1570. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00531-019-01719-5\nNdime, E. N., Ganno, S., Soh Tamehe, L., et al., 2018. Petrography, Lithostratigraphy and Major Element Geochemistry of Mesoarchean Metamorphosed Banded Iron Formation-Hosted Nkout Iron Ore Deposit, North Western Congo Craton, Central West Africa. Journal of African Earth Sciences, 148: 80–98. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jafrearsci.2018.06.007\nNielsen, R. L., Forsythe, L. M., Gallahan, W. E., et al., 1994. Major- and Trace-Element Magnetite-Melt Equilibria. Chemical Geology, 117(1\u002F2\u002F3\u002F4): 167–191. https:\u002F\u002Fdoi.org\u002F10.1016\u002F0009-2541(94)90127-9\nNzepang Tankwa, M., Ganno, S., Okunlola, O. A., et al., 2021. Petrogenesis and Tectonic Setting of the Paleoproterozoic Kelle Bidjoka Iron Formations, Nyong Group Greenstone Belts, Southwestern Cameroon. Constraints from Petrology, Geochemistry, and LA-ICP-MS Zircon U-Pb Geochronology. International Geology Review, 63(14): 1737–1757. https:\u002F\u002Fdoi.org\u002F10.1080\u002F00206814.2020.1793423\nRosière, C. A., Santos, J. O. S., Silveira Braga, F., et al., 2021. Multiple Hydrothermal Iron-Formation Upgrading Events in Southeastern São Francisco Craton. Journal of Geology, 129(3): 283–296. https:\u002F\u002Fdoi.org\u002F10.1086\u002F715242\nRudnick, R. L., Gao, S., 2003. Composition of the Continental Crust. Treatise on Geochemistry. Elsevier, Amsterdam. 1–64. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fb0-08-043751-6\u002F03016-4\nSilveira Braga, F. C., Rosière, C. A., Schneider Santos, J. O., et al., 2021. Geochemical and Tectonic Constraints on the Genesis of Iron Formation-Hosted Magnetite-Hematite Deposits at the Guanhães Block (Brazil) by Contact Metasomatism with Pegmatite Intrusions. Ore Geology Reviews, 129: 103931. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2020.103931\nSoh Tamehe, L., 2020. Geology and Genesis of the Gouap Banded Iron Formation (BIF)-Hosted Iron Deposit, South Cameroon: [Dissertation]. China University of Mining and Technology, Xuzhou\nSoh Tamehe, L., Nzepang Tankwa, M., Wei, C. T., et al., 2018. Geology and Geochemical Constrains on the Origin and Depositional Setting of the Kpwa-Atog Boga Banded Iron Formations (BIFs), Northwestern Congo Craton, Southern Cameroon. Ore Geology Reviews, 95: 620–638. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2018.03.017\nSoh Tamehe, L., Wei, C. T., Ganno, S., et al., 2019. Geology of the Gouap Iron Deposit, Congo Craton, Southern Cameroon: Implications for Iron Ore Exploration. Ore Geology Reviews, 107: 1097–1128. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2019.03.034\nSoh Tamehe, L., Wei, C. T., Ganno, S., et al., 2021. Depositional Age and Tectonic Environment of the Gouap Banded Iron Formations from the Nyong Group, SW Cameroon: Insights from Isotopic, Geochemical and Geochronological Studies of Drillcore Samples. Geoscience Frontiers, 12(2): 549–572. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.gsf.2020.07.009\nSoh Tamehe, L., Wei, C. T., Ganno, S., et al., 2022. Provenance of Metasiliciclastic Rocks at the Northwestern Margin of the East Gabonian Block: Implications for Deposition of BIFs and Crustal Evolution in Southwestern Cameroon. Precambrian Research, 376: 106677. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.precamres.2022.106677\nSong, Z., Li, H. M., Li, L. X., et al., 2021. Iron Isotopes and Trace Element Compositions of Magnetite from the Submarine Volcanic-Hosted Iron Deposits in East Tianshan, NW China: New Insights into the Mineralization Processes. Journal of Earth Science, 32(1): 219–234. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12583-020-1060-0\nSpier, C. A., de Oliveira, S. M. B., Rosière, C. A., et al., 2008. Mineralogy and Trace-Element Geochemistry of the High-Grade Iron Ores of the Águas Claras Mine and Comparison with the Capão Xavier and Tamanduá Iron Ore Deposits, Quadrilátero Ferrífero, Brazil. Mineralium Deposita, 43(2): 229–254. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00126-007-0157-z\nSun, X. H., Zhu, X. Q., Tang, H. S., et al., 2017. In situ LA-ICP-MS Trace Element Analysis of Magnetite from the Late Neoarchean Gongchangling BIFs, NE China: Constraints on the Genesis of High-Grade Iron Ore. Geological Journal, 53(S1): 8–20. https:\u002F\u002Fdoi.org\u002F10.1002\u002Fgj.3004\nSun, Z. Y., Wang, Y. W., Long, L. L., 2020. In-situ LA-ICP-MS Trace Element and Oxygen Isotope Signatures of Magnetite from the Yamansu Deposit, NW China, and Their Significance. Acta Geochimica, 39(5): 599–615. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11631-020-00418-2\nSwiffa Fajong, I., Nzepang Tankwa, M., Fossi, D. H., et al., 2022. Lithostratigraphy, Origin, and Geodynamic Setting of Iron Formations and Host Rocks of the Anyouzok Region, Congo Craton, Southwestern Cameroon. Minerals, 12(10): 1198. https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin12101198\nTeutsong, T., Bontognali, T. R. R., Ndjigui, P. D., et al., 2017. Petrography and Geochemistry of the Mesoarchean Bikoula Banded Iron Formation in the Ntem Complex (Congo Craton), Southern Cameroon: Implications for Its Origin. Ore Geology Reviews, 80: 267–288. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2016.07.003\nTeutsong, T., Temga, J. P., Enyegue, A. A., et al., 2021. Petrographic and Geochemical Characterization of Weathered Materials Developed on BIF from the Mamelles Iron Ore Deposit in the Nyong Unit, South-West Cameroon. Acta Geochimica, 40(2): 163–175. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11631-020-00421-7\nToteu, S. F., Van Schmus, W. R., Penaye, J., et al., 1994. U-Pb and Sm-N Edvidence for Eburnian and Pan-African High-Grade Metamorphism in Cratonic Rocks of Southern Cameroon. Precambrian Research, 67(3\u002F4): 321–347. https:\u002F\u002Fdoi.org\u002F10.1016\u002F0301-9268(94)90014-0\nToth, J., 1980. Deposition of Submarine Crusts Rich in Manganese and Iron. Geological Society of America Bulletin, 91: 44–54. https:\u002F\u002Fdoi.org\u002F10.1130\u002F0016-7606(1980)9144:DOSCRI>2.0.CO;2\nTrendall, A. F., 2002. The Significance of Iron-Formation in the Precambrian Stratigraphic Record. In: Altermann, W., Corcoran, P. L., eds., Precambrian Sedimentary Environments: A Modern Approach to Ancient Depositional Systems. Blackwell Publishing Ltd., Oxford. 33–66. https:\u002F\u002Fdoi.org\u002F10.1002\u002F9781444304312.ch3\nTsoungui, P. N. E., Ganno, S., Njiosseu, E. L. T., et al., 2020. Geochemical Constraints on the Origin and Tectonic Setting of the Serpentinized Peridotites from the Paleoproterozoic Nyong Series, Eseka Area, SW Cameroon. Acta Geochimica, 39(3): 404–422. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs11631-019-00368-4\nVerlaguet, A., Brunet, F., Goffé, B., et al., 2006. Experimental Study and Modeling of Fluid Reaction Paths in the Quartz-Kyanite ± Muscovite-Water System at 0.7 GPa in the 350–550 ·C Range: Implications for Al Selective Transfer during Metamorphism. Geochimica et Cosmochimica Acta, 70(7): 1772–1788. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.gca.2005.12.014\nWang, C. L., Konhauser, K. O., Zhang, L. C., 2015. Depositional Environment of the Paleoproterozoic Yuanjiacun Banded Iron Formation in Shanxi Province, China. Economic Geology, 110(6): 1515–1539. https:\u002F\u002Fdoi.org\u002F10.2113\u002Fecongeo.110.6.1515\nZhao, L. D., Chen, H. Y., Zhang, L., et al., 2018. Magnetite Geochemistry of the Heijianshan Fe-Cu (-Au) Deposit in Eastern Tianshan: Metallogenic Implications for Submarine Volcanic-Hosted Fe-Cu Deposits in NW China. Ore Geology Reviews, 100: 422–440. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2016.07.022\nZhou, Z. J., Tang, H. S., Chen, Y. J., et al., 2017. Trace Elements of Magnetite and Iron Isotopes of the Zankan Iron Deposit, Westernmost Kunlun, China: A Case Study of Seafloor Hydrothermal Iron Deposits. Ore Geology Reviews, 80: 1191–1205. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2016.09.020",{"EN":1549},"The Bipindi iron ore district is located in the central section of the Nyong Complex at the northwestern margin of the Congo Craton in Southwest Cameroon. This iron district contains numerous iron mineralization hosted by the Mewongo, Bibole, Kouambo, and Zambi banded iron formations (BIFs). These BIFs contain magnetite as the main iron ore mineral associated with pyrite, and gangue minerals are quartz with minor chlorite and amphibole. The origin of iron ore from these BIFs was investigated using a combination of in-situ magnetite and whole-rock chemistry. The studied BIF ore samples have a narrow range of TFe between 30.90 wt.% and 43.20 wt.%, indicating a low-grade ore. The geochemical signatures of magnetite such as low contents of base metals (e.g., Cu, Co, V, and Zn) and low Co\u002FZn ratios \u003C 0.85 indicate a hydrothermal origin. Combined with the geochemical features of these BIFs, e. g., high Fe\u002FTi and Fe\u002FAl ratios (mean > 600 and > 75, respectively), we suggest that magnetite was derived from a mixture of seawater and ∼0.1% low-temperature hydrothermal fluids in an oxidizing environment. Collectively, low-temperature hydrothermal and later metamorphic fluids were necessary for the transformation of the protolith Nyong Complex BIFs to iron ore.",{"EN":1551},"Insight into the Origin of Iron Ore Based on Elemental Contents of Magnetite and Whole-Rock Geochemistry: A Case of the Bipindi Banded Iron Formations, Nyong Complex, SW Cameroon",{"VOID":1553},"10.1007\u002Fs12583-022-1622-4","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12583-022-1622-4",[1556,1573,1588,1603,1615,1627],{"id":1557,"sortIndex":568,"researcher":20,"roles":1558,"affiliations":1559,"properties":1570},"8576f6c3-1e70-4117-bc3c-f14252e290fe",[570],[1560],{"id":20,"sortIndex":21,"affiliation":1561,"properties":20},{"id":1562,"createTime":1563,"updateTime":1564,"relativeEntities":1565,"slug":1566,"properties":1567,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"4b5bbd89-a707-4063-8f27-3a85b1eb565b","2023-12-02T05:08:06.878+00:00","2024-10-16T11:24:23.122+00:00",[],"School-of-Geosciences-and-Info-Physics-Central-South-University-Changsha-China",{"title":1568},{"VI":1569},"School of Geosciences and Info-Physics, Central South University, Changsha, China",{"title":1571},{"VI":1572},"Yanick Brice Lemdjou",{"id":1574,"sortIndex":711,"researcher":20,"roles":1575,"affiliations":1576,"properties":1585},"6a27eca0-518d-4389-ae4d-2a384defb124",[570],[1577],{"id":20,"sortIndex":21,"affiliation":1578,"properties":20},{"id":1579,"createTime":1580,"updateTime":1580,"relativeEntities":1581,"slug":20,"properties":1582,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"3a094f44-7440-4540-b5f1-70b4905ecf10","2024-02-18T23:49:20.875+00:00",[],{"title":1583},{"VI":1584},"Department of Geology, Ahmadu Bello University Zaria, Zaria, Nigeria",{"title":1586},{"VI":1587},"Safiyanu Muhammad Elatikpo",{"id":1589,"sortIndex":142,"researcher":20,"roles":1590,"affiliations":1591,"properties":1600},"b240ed8f-40d0-4ae2-92cd-8e35e4059815",[570],[1592],{"id":20,"sortIndex":21,"affiliation":1593,"properties":20},{"id":1594,"createTime":1595,"updateTime":1595,"relativeEntities":1596,"slug":20,"properties":1597,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"23e8e940-6cee-4aa0-ac61-3c5a1dbe9d25","2023-12-07T06:19:16.858+00:00",[],{"title":1598},{"VI":1599},"Department of Earth Sciences, University of Yaoundé I, Yaoundé, Cameroon",{"title":1601},{"VI":1602},"Sylvestre Ganno",{"id":1604,"sortIndex":21,"researcher":20,"roles":1605,"affiliations":1606,"properties":1612},"db24a7cd-06e4-42b6-a3ad-618b3c2dfd26",[570],[1607],{"id":20,"sortIndex":21,"affiliation":1608,"properties":20},{"id":1562,"createTime":1563,"updateTime":1564,"relativeEntities":1609,"slug":1566,"properties":1610,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":1611},{"VI":1569},{"title":1613},{"VI":1614},"Landry Soh Tamehe",{"id":1616,"sortIndex":206,"researcher":20,"roles":1617,"affiliations":1618,"properties":1624},"992fbf50-0521-4928-99fb-4c52077c343b",[570],[1619],{"id":20,"sortIndex":21,"affiliation":1620,"properties":20},{"id":1562,"createTime":1563,"updateTime":1564,"relativeEntities":1621,"slug":1566,"properties":1622,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":1623},{"VI":1569},{"title":1625},{"VI":1626},"Huan Li",{"id":1628,"sortIndex":52,"researcher":20,"roles":1629,"affiliations":1630,"properties":1641},"c67eb6ef-30fa-40bd-b12f-85f8162e69a4",[570],[1631],{"id":20,"sortIndex":21,"affiliation":1632,"properties":20},{"id":1633,"createTime":1634,"updateTime":1635,"relativeEntities":1636,"slug":1637,"properties":1638,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"095afe7f-5e63-43c1-aa3a-d2e798d6ab4d","2023-12-28T07:36:07.821+00:00","2025-06-11T22:18:12.755+00:00",[],"Institute-of-Oceanology-Chinese-Academy-of-Sciences-Qingdao-China",{"title":1639},{"VI":1640},"Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China",{"title":1642},{"VI":1643},"Zuxing 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A., Malinowski, M., Górszczyk, A., 2015. Full-Waveform Inversion of Conventional Vibroseis Data Recorded along a Regional Profile from Southeast Poland. Geophysical Journal International, 203(1): 351–365. https:\u002F\u002Fdoi.org\u002F10.1093\u002Fgji\u002Fggv305\nAlford, R. M., Kelly, K. R., Boore, D. M., 1974. Accuracy of Finite— Difference Modeling of the Acoustic Wave Equation. Geophysics, 39(6): 834–842. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1440470\nBerenger, J. P., 1994. A Perfectly Matched Layer for the Absorption of Electromagnetic Waves. Journal of Computational Physics, 114(2): 185–200. https:\u002F\u002Fdoi.org\u002F10.1006\u002Fjcph.1994.1159\nBian, A. F., Zou, Z. H., Zhou, H. W., et al., 2015. Evaluation of Multi-Scale Full Waveform Inversion with Marine Vertical Cable Data. Journal of Earth Science, 26(4): 481–486. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12583-015-0566-3\nBoonyasiriwat, C., Valasek, P., Routh, P., et al., 2009. An Efficient Multiscale Method for Time-Domain Waveform Tomography. Geophysics, 74(6): WCC59–WCC68. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.3151869\nBunks, C., Saleck, F. M., Zaleski, S., et al., 1995. Multiscale Seismic Waveform Inversion. Geophysics, 60(5): 1457–1473. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1443880\nCrase, E., Wideman, C., Noble, M., et al., 1992. Nonlinear Elastic Waveform Inversion of Land Seismic Reflection Data. Journal of Geophysical Research, 97(B4): 4685–4703. https:\u002F\u002Fdoi.org\u002F10.1029\u002F90jb00832\nDai, Y. H., Yuan, Y., 1999. A Nonlinear Conjugate Gradient Method with a Strong Global Convergence Property. SIAM Journal on Optimization, 10(1): 177–182. https:\u002F\u002Fdoi.org\u002F10.1137\u002Fs1052623497318992\nFletcher, R., Reeves, C. M., 1964. Function Minimization by Conjugate Gradients. The Computer Journal, 7(2): 149–154. https:\u002F\u002Fdoi.org\u002F10.1093\u002Fcomjnl\u002F7.2.149\nHager, W. W., Zhang, H. C., 2005. A New Conjugate Gradient Method with Guaranteed Descent and an Efficient Line Search. SIAM Journal on Optimization, 16(1): 170–192. https:\u002F\u002Fdoi.org\u002F10.1137\u002F030601880\nHager, W. W., Zhang, H. C., 2006. A Survey of Nonlinear Conjugate Gradient Methods. Pacific Journal of Optimization, 2(1): 35–58\nHanafy, S. M., Yu, H., 2013. Early Arrival Waveform Inversion of Shallow Seismic Land Data. SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists. 1738–1742. https:\u002F\u002Fdoi.org\u002F10.1190\u002Fsegam2013-0351.1\nHestenes, M. R., Stiefel, E., 1952. Methods of Conjugate Gradients for Solving Linear Systems. Journal of Research of the National Bureau of Standards, 49(6): 409–436. https:\u002F\u002Fdoi.org\u002F10.6028\u002Fjres.049.044\nKamei, R., Pratt, R. G., 2012. Wide-Band Multifrequency Waveform Inversion in the Laplace-Fourier Domain. SEG Technical Program Expanded Abstracts 2012. Society of Exploration Geophysicists. 1–6. https:\u002F\u002Fdoi.org\u002F10.1190\u002Fsegam2012-1588.1\nKim, Y., Cho, H., Min, D. J., et al., 2011. Comparison of Frequency-Selection Strategies for 2D Frequency-Domain Acoustic Waveform Inversion. Pure and Applied Geophysics, 168(10): 1715–1727. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00024-010-0196-8\nKomatitsch, D., Tromp, J., 2003. A Perfectly Matched Layer Absorbing Boundary Condition for the Second-Order Seismic Wave Equation. Geophysical Journal International, 154(1): 146–153. https:\u002F\u002Fdoi.org\u002F10.1046\u002Fj.1365-246x.2003.01950.x\nLevander, A. R., 1988. Fourth-Order Finite-Difference P-SV Seismograms. Geophysics, 53(11): 1425–1436. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1442422\nLiu, L., Ding, R. W., Liu, H. W., et al., 2015. 3D Hybrid-Domain Full Waveform Inversion on GPU. Computers & Geosciences, 83: 27–36. https:\u002F\u002Fdoi.org\u002F10.13039\u002F501100001809\nLiu, Y., Li, C. C., Mou, Y. G., 1998. Finite-Difference Numerical Modeling of any even Order Accuracy. Oil Geophysical Prospecting, 33(1): 1–10 (in Chinese with English Abstract)\nLiu, Y., Sen, M. K., 2009. A New Time-Space Domain High-Order Finite-Difference Method for the Acoustic Wave Equation. Journal of Computational Physics, 228(23): 8779–8806. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jcp.2009.08.027\nLuo, Y., Schuster, G. T., 1991. Wave-Equation Traveltime Inversion. Geophysics, 56(5): 645–653. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1443081\nMalinowski, M., Operto, S., Ribodetti, A., 2011. High-Resolution Seismic At tenuation Imaging from Wide-Aperture Onshore Data by Visco-Acoustic Frequency-Domain Full-Waveform Inversion. Geophysical Journal International, 186(3): 1179–1204. https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1365-246x.2011.05098.x\nMora, P., 1987. Nonlinear Two-Dimensional Elastic Inversion of Multioffset Seismic Data. Geophysics, 52(9): 1211–1228. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1442384\nPlessix, R. E., 2006. A Review of the Adjoint-State Method for Computing the Gradient of a Functional with Geophysical Applications. Geophysical Journal International, 167(2): 495–503. https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1365-246x.2006.02978.x\nPolak, E., Ribiere, G., 1969. Note Sur La Convergence de Méthodes de Directions Conjuguées. Revue Française d’Informatique et de Recherche opéRationnelle Série Rouge, 3(16): 35–43. https:\u002F\u002Fdoi.org\u002F10.1051\u002Fm2an\u002F196903r100351\nPowell, M. J. D., 1975. Convergence Properties of a Class of Minimization Algorithms. Nonlinear Programming, 2: 1–27. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fb978-0-12-468650-2.50005-5\nPratt, R. G., 1999. Seismic Waveform Inversion in the Frequency Domain, Part 1: Theory and Verification in a Physical Scale Model. Geophysics, 64(3): 888–901. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1444597\nQi, Q., Geers, T. L., 1998. Evaluation of the Perfectly Matched Layer for Computational Acoustics. Journal of Computational Physics, 139(1): 166–183. https:\u002F\u002Fdoi.org\u002F10.1006\u002Fjcph.1997.5868\nRavaut, C., Operto, S., Improta, L., et al., 2004. Multiscale Imaging of Complex Structures from Multifold Wide-Aperture Seismic Data by Frequency-Domain Full-Waveform Tomography: Application to a Thrust Belt. Geophysical Journal International, 159(3): 1032–1056. https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1365-246x.2004.02442.x\nShen, X., 2010. Near-Surface Velocity Estimation by Weighted Early-Arrival Waveform Inversion. SEG Technical Program Expanded Abstracts 2010. Society of Exploration Geophysicists. 1975–1979. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.3513230\nSheng, J., Leeds, A., Buddensiek, M., et al., 2006. Early Arrival Waveform Tomography on Near-Surface Refraction Data. Geophysics, 71(4): U47–U57. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.2210969\nShi, T. K., Zhang, J. Z., Huang, Z. L., et al., 2015. A Layer-Stripping Method for 3D Near-Surface Velocity Model Building Using Seismic First-Arrival Times. Journal of Earth Science, 26(4): 502–507. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12583-015-0569-0\nSirgue, L., Pratt, R. G., 2004. Efficient Waveform Inversion and Imaging: A Strategy for Selecting Temporal Frequencies. Geophysics, 69(1): 231–248. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1649391\nSirgue, L., Etgen, J. T., 2008. Albertin U. 3D Frequency Domain Waveform Inversion Using Time Domain Finite Difference Methods. 70th EAGE Conference and Exhibition Incorporating SPE EUROPEC 2008. https:\u002F\u002Fdoi.org\u002F10.3997\u002F2214-4609.20147683\nSong, Z. M., Williamson, P. R., Pratt, R. G., 1995. Frequency-Domain Acoustic-Wave Modeling and Inversion of Crosshole Data: Part II—Inversion Method, Synthetic Experiments and Real-Data Results. Geophysics, 60(3): 796–809. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1443818\nTarantola, A., 1987. Inverse Problem Theory: Methods for Data Fitting and Parameter Estimation. Society for Industrial & Applied Mathematics, Philadelphia. 342\nVirieux, J., Operto, S., 2009. An Overview of Full-Waveform Inversion in Exploration Geophysics. Geophysics, 74(6): WCC1–WCC26. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.3238367\nXu, K., McMechan, G. A., 2014. 2D Frequency-Domain Elastic Full-Waveform Inversion Using Time-Domain Modeling and a Multistep-Length Gradient Approach. Geophysics, 79(2): R41–R53. https:\u002F\u002Fdoi.org\u002F10.1190\u002Fgeo2013-0134.1\nYu, H., Hanafy, S. M., 2014. An Application of Multiscale Early Arrival Waveform Inversion to Shallow Seismic Data. Near Surface Geophysics, 12(4): 549–557. https:\u002F\u002Fdoi.org\u002F10.3997\u002F1873-0604.2014002\nZhang, J. Z., Huang, Y. Q., Song, L. P., et al., 2011. Fast and Accurate 3-D Ray Tracing Using Bilinear Traveltime Interpolation and the Wave Front Group Marching. Geophysical Journal International, 184(3): 1327–1340. https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1365-246x.2010.04909.x\nZhang, J. Z., Shi, T. K., Zhao, Y. S., et al., 2014. Static Corrections in Mountainous Areas Using Fresnel-Wavepath Tomography. Journal of Applied Geophysics, 111: 242–249. https:\u002F\u002Fdoi.org\u002F10.13039\u002F501100001809\nZhang, J. Z., Liu, H., Zou, Z. H., et al., 2015. Velocity Modeling and Inversion Techniques for Locating Microseismic Events in Unconventional Reservoirs. Journal of Earth Science, 26(4): 495–501. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12583-015-0565-4\nZhou, C. X., Cai, W. Y., Luo, Y., et al., 1995. Acoustic Wave-Equation Traveltime and Waveform Inversion of Crosshole Seismic Data. Geophysics, 60(3): 765–773. https:\u002F\u002Fdoi.org\u002F10.1190\u002F1.1443815",{"EN":1690},"Early-arrival waveform tomography (EWT) is one of the most promising techniques for building near-surface velocity model. Based on finite-frequency wave equation, EWT estimates velocities by matching calculated early-arrival waveforms with the observed ones. However, the objective function of EWT can easily converge to local minimum because of the cycle-skipping phenomenon. In order to reduce the cycle-skipping problem, a hybrid-domain early-arrival waveform tomography (HEWT) is proposed in this paper. The forward modeling of HEWT is realized in the time domain where early-arrival waveforms are easier to be selected from seismic data and less memory is needed than they are in the frequency domain. The inversion is implemented in the frequency domain where multi-scale strategy is more convenient to be realized than that in the time domain. Discrete Fourier transformation (DFT) is used to transform the time-domain wavefield to the frequency-domain wavefield. Test results show that HEWT is more competitive than EWT in both accuracy and computational time.",{"EN":1692},"Frequency-Domain Multi-Scale Early-Arrival Waveform Tomography with a Time-Domain Wavefield Modeling Engine",{"VOID":1694},"10.1007\u002Fs12583-018-0828-y","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12583-018-0828-y",[1697,1712,1724,1746],{"id":1698,"sortIndex":206,"researcher":20,"roles":1699,"affiliations":1700,"properties":1709},"8de2c108-4be9-4321-81f8-e69ea27e9b83",[570],[1701],{"id":20,"sortIndex":21,"affiliation":1702,"properties":20},{"id":1703,"createTime":1704,"updateTime":1704,"relativeEntities":1705,"slug":20,"properties":1706,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},"152d58b9-80c5-4529-9da1-904f658dece3","2023-12-09T06:50:10.656+00:00",[],{"title":1707},{"VI":1708},"Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of 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Qingdao National Laboratory for Marine Science and Technology, Qingdao, China",{},{"title":1744},{"VI":1745},"Jianzhong Zhang",{"id":1747,"sortIndex":142,"researcher":20,"roles":1748,"affiliations":1749,"properties":1755},"798be1a6-38df-4563-a556-025c04572e2b",[570],[1750],{"id":20,"sortIndex":21,"affiliation":1751,"properties":20},{"id":1703,"createTime":1704,"updateTime":1704,"relativeEntities":1752,"slug":20,"properties":1753,"entityType":41,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"syncStatus":19,"languages":20,"translateLanguages":20,"viewCount":21},[],{"title":1754},{"VI":1708},{"title":1756},{"VI":1757},"Taikun 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