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Soc., 142, 1159, 10.1144\u002Fgsjgs.142.6.1159",{"doi":352},"10.1144\u002Fgsjgs.142.6.1159",{"id":24,"text":354,"url":24,"identifiers":355},"Darbyshire, 1994, Nd and Sr isotope constraints on the origin of the Cornubian batholith, SW England, Jour. Geol. Soc., 151, 795, 10.1144\u002Fgsjgs.151.5.0795",{"doi":356},"10.1144\u002Fgsjgs.151.5.0795",{"id":24,"text":358,"url":24,"identifiers":359},"Davies, 1985, Upper crustal recycling in southern Britain: evidence from Nd and Sr isotopes, Earth Planet. Sci. Lett., 75, 1, 10.1016\u002F0012-821X(85)90045-7",{"doi":360},"10.1016\u002F0012-821X(85)90045-7",{"id":24,"text":362,"url":24,"identifiers":363},"Edmonds, 1968, Geology of the Country Around Okehampton",{},{"id":24,"text":365,"url":24,"identifiers":366},"Edmondson, K. M. (1972) Some Aspects of the Chemistry of the Bodmin Moor Granite. PhD Thesis, Univ. 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Acta., 58, 4127, 10.1016\u002F0016-7037(94)90269-0",{"doi":659},"10.1016\u002F0016-7037(94)90269-0",{"id":24,"text":661,"url":24,"identifiers":662},"Wyborn, 1998, Compositional changes during fractionation of felsic granites from western Tasmania, Australia, Acta Univ. Carolinae Geol., 42, 189",{},false,{"id":665,"createTime":666,"updateTime":666,"relativeEntities":667,"slug":668,"properties":669,"entityType":140,"verifyStatus":141,"verifyTime":666,"verifyNote":142,"syncStatus":23,"languages":681,"translateLanguages":24,"viewCount":25,"primaryUrl":682,"fullTextUrl":24,"authors":683,"publicationType":185,"publisherRelationship":705,"citationCount":742,"citationInfo":743,"publishDate":745,"publishYear":746,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":747,"isForceReanalyzing":663},"e2262ae0-2b03-411b-b911-d68fbc698b85","2025-02-09T15:34:11.291+00:00",[],"Regional-Exploration-Targeting-Model-for-Gangdese-Porphyry-Copper-Deposits",{"mag":670,"keywords":672,"openalex":673,"abstract":675,"title":677,"doi":679},{"VOID":671},"1542116403",{},{"VOID":674},"W1542116403",{"EN":676},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>An exploration targeting model for Gangdese porphyry copper deposit in Tibet, China, is constructed based on (i) the age of porphyry intrusions within Gangdese magmatic arc; (ii) the regional‐scale normal E–W, N–S and N–E striking faults; and (iii) comprehensive anomalously high concentrations of Cu‐Mo‐Au‐Ag‐Pb‐Zn. These targeting elements are derived from geological map and geochemical dataset, and are integrated by weights of evidence with the aid of geographic information system (GIS). The resulting prospectivity for porphyry copper deposits delineated by posterior probability demonstrates that the target areas extend along the Yaluzangbujiang River and contain the two large deposits, Qulong and Chongjiang, located in the eastern and central part of the Gangdese belt, respectively. These results indicate that the proposed exploration targeting model is a potential tool to map regional‐scale mineral prospectivity. The target areas with high values of favorability, especially where high concentrations of Cu‐Mo‐Au‐Ag‐Pb‐Zn are present, are the potential areas for finding undiscovered porphyry copper deposits.\u003C\u002Fjats:p>",{"EN":678},"Regional Exploration Targeting Model for Gangdese Porphyry Copper Deposits",{"VOID":680},"10.1111\u002Fj.1751-3928.2011.00166.x",[144],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1751-3928.2011.00166.x",[684],{"id":685,"sortIndex":25,"researcher":24,"roles":686,"affiliations":687,"properties":698},"7a71b70f-0b59-4d92-8978-6d04701d9690",[],[688],{"id":689,"sortIndex":25,"affiliation":690,"properties":24},"5d67e1d5-2c2a-44be-af02-c2083ef83eba",{"id":691,"createTime":692,"updateTime":692,"relativeEntities":693,"slug":694,"properties":695,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"2e1b06d9-2390-44cf-a742-f2db7f22892f","2025-02-09T15:34:11.312+00:00",[],"State-Key-Laboratory-of-Geological-Processes-and-Mineral-Resources-China-University-of-Geosciences-Wuhan-Beijing-China",{"title":696},{"EN":697},"State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Beijing, China",{"openalex":699,"orcid":701,"title":703},{"VOID":700},"A5008183305",{"VOID":702},"https:\u002F\u002Forcid.org\u002F0000-0002-5639-3128",{"EN":704},"Renguang Zuo",{"url":24,"publisher":706,"properties":736},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":707,"slug":10,"properties":708,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":714,"manageAffiliations":715,"indexDatabases":716,"url":106,"thumbnailPath":24,"statistic":731,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":709,"issn":710,"introduce":711,"eissn":712,"title":713},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[717,724],{"id":87,"indexDatabase":718,"url":102,"indexYears":24,"academicFieldIds":723,"indexDatabaseRanking":24},{"id":89,"createTime":90,"updateTime":91,"relativeEntities":719,"label":720,"description":721,"key":98,"publicationTags":722,"standard":24},[],{"EN":94,"VI":94},{"VI":96,"EN":97},[100,101],[104,105],{"id":67,"indexDatabase":725,"url":80,"indexYears":81,"academicFieldIds":730,"indexDatabaseRanking":85},{"id":69,"createTime":70,"updateTime":71,"relativeEntities":726,"label":727,"description":728,"key":77,"publicationTags":729,"standard":24},[],{"EN":74,"VI":74},{"EN":74,"VI":76},[79],[83,84],{"impactFactor":25,"impactFactorByYear":732,"i10Index":111,"i10IndexLast5Year":25,"totalPublication":111,"totalPublicationByYear":733,"totalCitation":114,"totalCitationByYear":734,"totalCitationPerPublication":118,"totalCitationPerPublicationByYear":735,"hindexLast5Year":111,"hindex":111},{"2012":109,"2013":110},{"2002":113,"2011":113},{"2002":116,"2011":117},{"2002":116,"2011":117},{"volume":737,"pages":739,"issue":741},{"VOID":738},"61",{"VOID":740},"296-303",{"VOID":223},17,{"total":742,"publishYear":24,"statisticByYear":744},{"2012":113,"2013":113,"2014":111,"2015":111,"2016":109,"2017":113,"2018":113,"2021":111,"2022":113},"2011-07-01",2011,[748,751,754,757,760,763,766,769,772,775,778,781,784,787,790,793,796,799,802,805,808,811,814,817,820,823,826,829,832,835,838,841,844,847,850,853,856,859,862,865,868],{"id":24,"text":749,"url":24,"identifiers":750},"Agterberg F. P.(1989)Systematic approach to dealing with uncertainty of geoscience information in mineral exploration. Proceedings of the 21st APCOM Symposium Las Vegas USA Chapter 18 p. 165–178.",{},{"id":24,"text":752,"url":24,"identifiers":753},"10.1038\u002F307017a0",{"doi":752},{"id":24,"text":755,"url":24,"identifiers":756},"10.1007\u002Fs00126-003-0375-y",{"doi":755},{"id":24,"text":758,"url":24,"identifiers":759},"10.1038\u002F35088045",{"doi":758},{"id":24,"text":761,"url":24,"identifiers":762},"Bonham‐Carter G. F., 1994, Geographic information systems for geoscientists: modeling with GIS, 398",{},{"id":24,"text":764,"url":24,"identifiers":765},"10.1038\u002F311219a0",{"doi":764},{"id":24,"text":767,"url":24,"identifiers":768},"10.1023\u002FB:NARR.0000046919.87758.f5",{"doi":767},{"id":24,"text":770,"url":24,"identifiers":771},"10.2113\u002Fgsecongeo.100.5.801",{"doi":770},{"id":24,"text":773,"url":24,"identifiers":774},"10.1016\u002F0012-821X(86)90186-X",{"doi":773},{"id":24,"text":776,"url":24,"identifiers":777},"Gao S., 2005, Study on the Geochemical characteristics and Metallogenic mechanism of Gangdise Porphyry Copper Deposits in Tibet",{},{"id":24,"text":779,"url":24,"identifiers":780},"Hou Z., 2001, Gangdese porphyry copper belt the second “yulong” copper belt, China Geol., 28, 27",{},{"id":24,"text":782,"url":24,"identifiers":783},"10.2113\u002F98.1.125",{"doi":782},{"id":24,"text":785,"url":24,"identifiers":786},"Hou Z., 2003, Adakite: a significant Cubearing porphyry‐a case study on porphyry Cu deposits in Tibet and northern Chile, Miner. Deposits, 22, 1",{},{"id":24,"text":788,"url":24,"identifiers":789},"Hou Z., 2003, Re–Os age for molybdenite from the Gangdese porphyry copper belt on Tibetan plateau: implication for geodynamic setting and duration of the Cu mineralization., Sci. China, 33, 509",{},{"id":24,"text":791,"url":24,"identifiers":792},"10.1016\u002FS0012-821X(04)00007-X",{"doi":791},{"id":24,"text":794,"url":24,"identifiers":795},"10.1016\u002Fj.oregeorev.2008.09.006",{"doi":794},{"id":24,"text":797,"url":24,"identifiers":798},"10.1126\u002Fscience.274.5293.1692",{"doi":797},{"id":24,"text":800,"url":24,"identifiers":801},"10.1046\u002Fj.1440-0952.2000.00816.x",{"doi":800},{"id":24,"text":803,"url":24,"identifiers":804},"Li G., 2004, Diagenetic and mineralization ages for the porphyry copper deposits in the gangdise metallogenic belt, southern Xizang, Geotectonica et Metallogenia, 28, 165",{},{"id":24,"text":806,"url":24,"identifiers":807},"Lord D., 2001, Measuring exploration success: an alternative to the discovery‐cost‐per‐ounce method of quantifying exploration effectiveness, SEG Newsl., 45, 10",{},{"id":24,"text":809,"url":24,"identifiers":810},"10.2113\u002Fgsecongeo.65.4.373",{"doi":809},{"id":24,"text":812,"url":24,"identifiers":813},"10.1093\u002Fpetroj\u002F40.9.1399",{"doi":812},{"id":24,"text":815,"url":24,"identifiers":816},"Qu X., 2001, Is Gangdese porphyry copper belt the second “yulong” copper belt?, Miner. Deposits, 20, 355",{},{"id":24,"text":818,"url":24,"identifiers":819},"Qu X., 2003, 40Ar\u002F39Ar ages of porphyries from the Gangdese porphyry Cu belt in south Tibet and implication to geodynamic setting, Acta Geol. Sin., 77, 245",{},{"id":24,"text":821,"url":24,"identifiers":822},"10.1016\u002Fj.oregeorev.2005.03.012",{"doi":821},{"id":24,"text":824,"url":24,"identifiers":825},"10.2113\u002Fgsecongeo.98.8.1515",{"doi":824},{"id":24,"text":827,"url":24,"identifiers":828},"Rui Z., 2003, Metallogenic epoch of Gangdese porphyry copper belt and uplift of Qinghai‐Tibetan Plateau, Miner. Deposits, 22, 224",{},{"id":24,"text":830,"url":24,"identifiers":831},"Rui Z., 2004, The response of porphyry copper deposits to important geological events in Xizang (Tibet), Earth Sci. Front., 11, 145",{},{"id":24,"text":833,"url":24,"identifiers":834},"10.2113\u002Fgsecongeo.67.2.184",{"doi":833},{"id":24,"text":836,"url":24,"identifiers":837},"Sillitoe R. H.(1993)Gold‐rich porphyry copper deposits: geological model and exploration implication. Mineral Deposit Modeling Geological Association of Canada Special Paper 40 465–478.",{},{"id":24,"text":839,"url":24,"identifiers":840},"10.1016\u002FS0375-6742(97)00029-0",{"doi":839},{"id":24,"text":842,"url":24,"identifiers":843},"10.1016\u002Fj.oregeorev.2009.03.003",{"doi":842},{"id":24,"text":845,"url":24,"identifiers":846},"10.1146\u002Fannurev.earth.28.1.211",{"doi":845},{"id":24,"text":848,"url":24,"identifiers":849},"Zheng Y., 2004, Finding, characteristics and significances of Qulong superlarge porphyry copper (molybdenum) deposit, Tibet, Earth Sci. J. China Univ. Geosci., 29, 103",{},{"id":24,"text":851,"url":24,"identifiers":852},"Zheng Y., 2004, Finding and significances of Chongjiang porphyry copper (molybdenum, aurum) deposit, Tibet, Earth Sci. J. China Univ. Geosci., 29, 333",{},{"id":24,"text":854,"url":24,"identifiers":855},"Zheng Y., 2006, The discovery of Zhunuo porphyry copper deposit in Tibet and its significance, Earth Sci. Front., 13, 233",{},{"id":24,"text":857,"url":24,"identifiers":858},"10.1007\u002Fs11434-007-0406-7",{"doi":857},{"id":24,"text":860,"url":24,"identifiers":861},"10.1180\u002Fminmag.2008.072.1.531",{"doi":860},{"id":24,"text":863,"url":24,"identifiers":864},"Zuo R., 2007, Synthetic information prediction of porphyry copper in Tibet, Cent. South Univ. Technol., 38, 368",{},{"id":24,"text":866,"url":24,"identifiers":867},"10.1016\u002Fj.oregeorev.2008.11.004",{"doi":866},{"id":24,"text":869,"url":24,"identifiers":870},"10.1016\u002Fj.gexplo.2008.08.003",{"doi":869},{"id":872,"createTime":873,"updateTime":873,"relativeEntities":874,"slug":875,"properties":876,"entityType":140,"verifyStatus":141,"verifyTime":888,"verifyNote":142,"syncStatus":23,"languages":889,"translateLanguages":24,"viewCount":25,"primaryUrl":890,"fullTextUrl":24,"authors":891,"publicationType":185,"publisherRelationship":947,"citationCount":116,"citationInfo":985,"publishDate":988,"publishYear":989,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":990,"isForceReanalyzing":663},"4678707f-04c8-47ee-8674-fac13a6e9d56","2024-10-03T07:08:31.726+00:00",[],"Geochemical-and-Nd-Sr-Isotopic-Study-of-the-Post-Orogenic-Granites-in-the-Yidun-Arc-Belt-of-Northern-Sanjiang-Region-Southwestern-China",{"mag":877,"keywords":879,"openalex":880,"abstract":882,"title":884,"doi":886},{"VOID":878},"2032340654",{},{"VOID":881},"W2032340654",{"EN":883},"\u003Cjats:p>\u003Cjats:bold>Abstract: \u003C\u002Fjats:bold> In the arc (basin)–back area of the Yidun arc belt in the north segment of the Sanjiang tectonic zone, southwestern China, there occurs a post‐orogenic granite belt extending for more than 300 km in NNW direction. It strides across two different tectonic units of the arc (basin)–back area and the subduction area, and is accompanied by extensive Ag‐Sn polymetal–lic mineralizations. More than ten granite bodies have very similar geochemical characteristics: high SiO\u003Cjats:sub>2\u003C\u002Fjats:sub> (73.8–76.3 wt%) and K\u003Cjats:sub>2\u003C\u002Fjats:sub>O+Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O (7.16‐8.41 %), and low Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> (11.9–13.6 %), CaO (0.46‐1.54 %) and MgO (0.16‐0.61 %), as well as high enrichment of Nb, Ta, Ga and Y, and strong depletion of Sr and Eu. Most of these features are peculiar to A‐type granite. Rb‐Sr and \u003Cjats:sup>40\u003C\u002Fjats:sup>Ar\u002F\u003Cjats:sup>39\u003C\u002Fjats:sup>Ar isotopic dating results indicate that the formation ages of the granites decrease from 103.7 Ma of the north end to 75.2 Ma near the south end, and that the magmatism became younger from north to south. The tectonic environment analysis clearly reveals that they were formed in post‐orogenic within–plate extension settings. The magma genesis was controlled by a united crustal extension regime after the arc‐continent collision. The granites have low \u003Cjats:sub>Nd\u003C\u002Fjats:sub> values ranging from –4.96 to –8.40, whereas the \u003Cjats:sub>Sr\u003C\u002Fjats:sub> values vary greatly ranging from –31.7 to 296, reflecting that the source composition transited from mantle – differentiated igneous rocks in the north to basement – dominated metamorphosed sedimentary rocks in the south. Under high temperature and water‐absent conditions, the anatexes of the crustal rocks made a great amount of plagioclase separated from melts and left in magma sources. Through this mechanism, the post‐orogenic granites took geo‐chemical characteristics such as low Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> and CaO, and strong depletion of Sr and Eu.\u003C\u002Fjats:p>",{"EN":885},"Geochemical and Nd, Sr Isotopic Study of the Post‐Orogenic Granites in the Yidun Arc Belt of Northern Sanjiang Region, Southwestern 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Baiwanzhuang Road 26, Beijing 100037, China [e-mail: imdcags@public3.bta.net.cn]",{"openalex":907,"title":909},{"VOID":908},"A5010194559",{"EN":910},"Xiaoming Qu",{"id":912,"sortIndex":113,"researcher":24,"roles":913,"affiliations":914,"properties":921},"47ece5bb-bd0c-46a5-b40c-0638739f04d8",[],[915],{"id":916,"sortIndex":25,"affiliation":917,"properties":24},"e1fd0edd-2c50-4f86-b716-f7281ce7419a",{"id":899,"createTime":900,"updateTime":900,"relativeEntities":918,"slug":902,"properties":919,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},[],{"title":920},{"EN":905},{"openalex":922,"title":924},{"VOID":923},"A5100932318",{"EN":925},"Zengqian 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Q., 1993, The tectono‐magmatic evolution of Yidun Island‐arc and geodynamic settings of the formation of Kuroko‐type massive sulphide deposits in Sanjiang region, S, W. China. Resource Geol., Spec. Issue, 17, 336",{},{"id":24,"text":1016,"url":24,"identifiers":1017},"Huang J. Q., 1986, The Evolution of Tethys Sea of China and the Neighbour Region",{},{"id":24,"text":1019,"url":24,"identifiers":1020},"10.1016\u002F0040-1951(93)90295-U",{"doi":1019},{"id":24,"text":1022,"url":24,"identifiers":1023},"10.1016\u002F0009-2541(93)90141-5",{"doi":1022},{"id":24,"text":1025,"url":24,"identifiers":1026},"Lu B. X., 1993, The Granitoids and Metallogenic Specialization in Sanjiang Region",{},{"id":24,"text":1028,"url":24,"identifiers":1029},"Mo X. X., 1993, The Volcanism and Metallogeny of Tethys in Sanjiang Region",{},{"id":24,"text":1031,"url":24,"identifiers":1032},"10.1093\u002Fpetrology\u002F25.4.956",{"doi":1031},{"id":24,"text":1034,"url":24,"identifiers":1035},"Qiu J. Y., 1985, Petrology of Magmatic Rocks",{},{"id":24,"text":1037,"url":24,"identifiers":1038},"Qu X. M., 2001, The characteristics and origin of Nongduke volcanic‐hosted epithermal Ag polymetallic deposit in western Sichuan Province, Mineral Deposits, 20, 199",{},{"id":24,"text":1040,"url":24,"identifiers":1041},"Qu X. M., 2001, Metallogenic geological characteristics of the Lianlong skarn‐type SnAg polymetallic deposit in western Sichuan Province, Acta Geosci. Sinica, 22, 29",{},{"id":24,"text":1043,"url":24,"identifiers":1044},"Shen W. Z., 1991, Nd, Sr, O isotopic and geological study of Xiqou spilite–keratophyre, Zhejiang Province, Acta Geol. Sinica, 337",{},{"id":24,"text":1046,"url":24,"identifiers":1047},"10.1130\u002F0091-7613(1992)020\u003C0263:VAMAKO>2.3.CO;2",{"doi":1046},{"id":24,"text":1049,"url":24,"identifiers":1050},"10.1007\u002FBF00402202",{"doi":1049},{"id":24,"text":1052,"url":24,"identifiers":1053},"Ye Q. T., 1991, The ore‐forming geological characteristics and the origin of Gacun auriferous rich‐Ag polymetallic deposit in Sichuan Province, Mineral Deposits, 10, 107",{},{"id":1055,"createTime":1056,"updateTime":1056,"relativeEntities":1057,"slug":1058,"properties":1059,"entityType":140,"verifyStatus":141,"verifyTime":1056,"verifyNote":142,"syncStatus":23,"languages":1071,"translateLanguages":24,"viewCount":25,"primaryUrl":1072,"fullTextUrl":24,"authors":1073,"publicationType":185,"publisherRelationship":1095,"citationCount":117,"citationInfo":1132,"publishDate":1136,"publishYear":746,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1137,"isForceReanalyzing":663},"d17acb80-e522-4bac-ae94-9224af0a12f5","2024-09-21T06:13:39.636+00:00",[],"From-Predictive-Mapping-of-Mineral-Prospectivity-to-Quantitative-Estimation-of-Number-of-Undiscovered-Prospects",{"mag":1060,"keywords":1062,"openalex":1063,"abstract":1065,"title":1067,"doi":1069},{"VOID":1061},"1882925433",{},{"VOID":1064},"W1882925433",{"EN":1066},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>This paper proposes that the spatial pattern of known prospects of the deposit‐type sought is the key to link predictive mapping of mineral prospectivity (PMMP) and quantitative mineral resource assessment (QMRA). This proposition is demonstrated by PMMP for hydrothermal Au‐Cu deposits (HACD) and by estimating the number of undiscovered prospects for HACD in Catanduanes Island (Philippines). The results of analyses of the spatial pattern of known prospects of HACD and their spatial associations with geological features are consistent with existing knowledge of geological controls on hydrothermal Au‐Cu mineralization in the island and elsewhere, and are used to define spatial recognition criteria of regional‐scale prospectivity for HACD. Integration of layers of evidence representing the spatial recognition criteria of prospectivity via application of data‐driven evidential belief functions results in a map of prospective areas occupying 20% of the island with fitting‐ and prediction‐rates of 76% and 70%, respectively. The predictive map of prospective areas and a proxy measure for degrees of exploration based on the spatial pattern of known prospects of HACD were used in one‐level prediction of undiscovered mineral endowment, which yielded estimates of 79 to 112 undiscovered prospects of HACD. Application of radial‐density fractal analysis of the spatial pattern of known prospects of HACD results in an estimate of 113 undiscovered prospects of HACD. Thus, the results of the study support the proposition that PMMP can be a part of QMRA if the spatial pattern of discovered prospects of the deposit‐type sought is considered in both PMMP and QMRA.\u003C\u002Fjats:p>",{"EN":1068},"From Predictive Mapping of Mineral Prospectivity to Quantitative Estimation of Number of Undiscovered Prospects",{"VOID":1070},"10.1111\u002Fj.1751-3928.2010.00146.x",[144],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1751-3928.2010.00146.x",[1074],{"id":1075,"sortIndex":25,"researcher":24,"roles":1076,"affiliations":1077,"properties":1088},"0d06f115-1046-4166-8088-872be237da5d",[],[1078],{"id":1079,"sortIndex":25,"affiliation":1080,"properties":24},"31f2b22f-54d4-4247-9265-ec0926574a05",{"id":1081,"createTime":1082,"updateTime":1082,"relativeEntities":1083,"slug":1084,"properties":1085,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"71ec486d-a6fa-40d9-a823-7cdeaf90ebcd","2024-09-21T06:13:39.652+00:00",[],"Department-of-Earth-Systems-Analysis-Faculty-of-Geo-Information-Science-and-Earth-Observation-ITC-University-of-Twente-Enschede-The-Netherlands",{"title":1086},{"EN":1087},"Department of Earth Systems Analysis, Faculty of Geo‐Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands",{"openalex":1089,"orcid":1091,"title":1093},{"VOID":1090},"A5007016189",{"VOID":1092},"https:\u002F\u002Forcid.org\u002F0000-0003-1765-0352",{"EN":1094},"Emmanuel John M. Carranza",{"url":24,"publisher":1096,"properties":1126},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1097,"slug":10,"properties":1098,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1104,"manageAffiliations":1105,"indexDatabases":1106,"url":106,"thumbnailPath":24,"statistic":1121,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1099,"issn":1100,"introduce":1101,"eissn":1102,"title":1103},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[1107,1114],{"id":87,"indexDatabase":1108,"url":102,"indexYears":24,"academicFieldIds":1113,"indexDatabaseRanking":24},{"id":89,"createTime":90,"updateTime":91,"relativeEntities":1109,"label":1110,"description":1111,"key":98,"publicationTags":1112,"standard":24},[],{"EN":94,"VI":94},{"VI":96,"EN":97},[100,101],[104,105],{"id":67,"indexDatabase":1115,"url":80,"indexYears":81,"academicFieldIds":1120,"indexDatabaseRanking":85},{"id":69,"createTime":70,"updateTime":71,"relativeEntities":1116,"label":1117,"description":1118,"key":77,"publicationTags":1119,"standard":24},[],{"EN":74,"VI":74},{"EN":74,"VI":76},[79],[83,84],{"impactFactor":25,"impactFactorByYear":1122,"i10Index":111,"i10IndexLast5Year":25,"totalPublication":111,"totalPublicationByYear":1123,"totalCitation":114,"totalCitationByYear":1124,"totalCitationPerPublication":118,"totalCitationPerPublicationByYear":1125,"hindexLast5Year":111,"hindex":111},{"2012":109,"2013":110},{"2002":113,"2011":113},{"2002":116,"2011":117},{"2002":116,"2011":117},{"volume":1127,"pages":1128,"issue":1130},{"VOID":738},{"VOID":1129},"30-51",{"VOID":1131},"1",{"total":117,"publishYear":24,"statisticByYear":1133},{"2012":109,"2013":110,"2014":1134,"2015":1135,"2016":227,"2017":109,"2018":109,"2019":63,"2020":110,"2021":227,"2022":110,"2023":227,"2024":111},7,12,"2011-01-01",[1138,1141,1144,1147,1150,1153,1156,1159,1162,1165,1169,1172,1175,1178,1181,1184,1187,1190,1193,1196,1199,1202,1205,1208,1211,1214,1217,1220,1223,1226,1229,1232,1235,1239,1242,1245,1248,1251,1254,1257,1260,1263,1266,1269,1272,1275,1278,1281,1284,1287,1290,1293,1296,1299,1302,1305,1308,1311,1314,1317,1320,1323,1326,1329,1332,1335,1338,1341,1344,1347,1350,1353,1356,1359,1362,1365,1368,1371,1374,1377,1380,1383,1386,1389,1392,1395,1398,1401,1404,1407,1410,1413],{"id":24,"text":1139,"url":24,"identifiers":1140},"10.1016\u002FB978-0-08-037245-7.50006-8",{"doi":1139},{"id":24,"text":1142,"url":24,"identifiers":1143},"Agterberg F. P., 1993, Computers in Geology, 13",{},{"id":24,"text":1145,"url":24,"identifiers":1146},"Agterberg F. P. Cheng Q.andWright D. F.(1993b)Fractal modeling of mineral deposits. Proceedings 24th APCOM Symposium Canadian Inst. Mining Metallurgy and Petroleum Engineers vol. 1 pp.43–53.",{},{"id":24,"text":1148,"url":24,"identifiers":1149},"10.1007\u002Fs11053-005-4674-0",{"doi":1148},{"id":24,"text":1151,"url":24,"identifiers":1152},"10.1007\u002FBF02261716",{"doi":1151},{"id":24,"text":1154,"url":24,"identifiers":1155},"10.1016\u002Fj.oregeorev.2009.03.004",{"doi":1154},{"id":24,"text":1157,"url":24,"identifiers":1158},"10.1007\u002F978-3-662-07304-9_19",{"doi":1157},{"id":24,"text":1160,"url":24,"identifiers":1161},"Blenkinsop T. G., 1995, Sub‐saharan economic geology, 177",{},{"id":24,"text":1163,"url":24,"identifiers":1164},"10.1111\u002Fj.1468-8123.2006.00154.x",{"doi":1163},{"id":24,"text":1166,"url":24,"identifiers":1167},"Blenkinsop T. 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F., 1989, Statistical Applications in the Earth Sciences, Geological Survey of Canada, Paper 89‐9, 171",{},{"id":24,"text":1185,"url":24,"identifiers":1186},"Boots B. N., 1988, point pattern analysis. Sage university scientific geography series no. 8",{},{"id":24,"text":1188,"url":24,"identifiers":1189},"10.1130\u002F0091-7613(1991)019\u003C0111:SDOOD>2.3.CO;2",{"doi":1188},{"id":24,"text":1191,"url":24,"identifiers":1192},"Carranza E. J. M., 2002, Geologically‐Constrained Mineral Potential Mapping (Examples from the Philippines). Phd Thesis, Delft University of Technology, The Netherlands",{},{"id":24,"text":1194,"url":24,"identifiers":1195},"Carranza E. J. M., 2008, Geochemical Anomaly and Mineral Prospectivity Mapping in GIS. Handbook of Exploration and Environmental Geochemistry",{},{"id":24,"text":1197,"url":24,"identifiers":1198},"10.1016\u002Fj.oregeorev.2009.01.001",{"doi":1197},{"id":24,"text":1200,"url":24,"identifiers":1201},"10.1144\u002F1467-7873\u002F09-223",{"doi":1200},{"id":24,"text":1203,"url":24,"identifiers":1204},"10.1016\u002Fj.cageo.2009.02.008",{"doi":1203},{"id":24,"text":1206,"url":24,"identifiers":1207},"10.1016\u002FS0375-6742(97)00032-0",{"doi":1206},{"id":24,"text":1209,"url":24,"identifiers":1210},"10.2113\u002F0100165",{"doi":1209},{"id":24,"text":1212,"url":24,"identifiers":1213},"10.1023\u002FA:1014416319335",{"doi":1212},{"id":24,"text":1215,"url":24,"identifiers":1216},"10.1016\u002FS0169-1368(02)00111-7",{"doi":1215},{"id":24,"text":1218,"url":24,"identifiers":1219},"10.1016\u002Fj.oregeorev.2010.02.003",{"doi":1218},{"id":24,"text":1221,"url":24,"identifiers":1222},"10.1007\u002Fs11053-005-4678-9",{"doi":1221},{"id":24,"text":1224,"url":24,"identifiers":1225},"10.1016\u002Fj.geothermics.2008.03.003",{"doi":1224},{"id":24,"text":1227,"url":24,"identifiers":1228},"10.1007\u002Fs00126-009-0250-6",{"doi":1227},{"id":24,"text":1230,"url":24,"identifiers":1231},"10.1007\u002FBF02087098",{"doi":1230},{"id":24,"text":1233,"url":24,"identifiers":1234},"10.1007\u002FBF02257585",{"doi":1233},{"id":24,"text":1236,"url":24,"identifiers":1237},"Chung C. F., 1980, Regression models for estimating mineral resources from geological map data, Math. Geol., 12, 472, 10.1007\u002FBF01028881",{"doi":1238},"10.1007\u002FBF01028881",{"id":24,"text":1240,"url":24,"identifiers":1241},"10.1007\u002FBF02272805",{"doi":1240},{"id":24,"text":1243,"url":24,"identifiers":1244},"10.1214\u002Faoms\u002F1177698950",{"doi":1243},{"id":24,"text":1246,"url":24,"identifiers":1247},"Dempster A. P., 1968, A generalization of Bayesian inference, J. R. Stat. Soc., 30, 205",{},{"id":24,"text":1249,"url":24,"identifiers":1250},"10.1007\u002FBF02272806",{"doi":1249},{"id":24,"text":1252,"url":24,"identifiers":1253},"10.1007\u002Fs11053-008-9072-y",{"doi":1252},{"id":24,"text":1255,"url":24,"identifiers":1256},"10.1016\u002Fj.oregeorev.2010.03.009",{"doi":1255},{"id":24,"text":1258,"url":24,"identifiers":1259},"10.1016\u002Fj.oregeorev.2007.01.004",{"doi":1258},{"id":24,"text":1261,"url":24,"identifiers":1262},"10.1016\u002Fj.oregeorev.2010.03.008",{"doi":1261},{"id":24,"text":1264,"url":24,"identifiers":1265},"10.1016\u002F0040-1951(79)90135-5",{"doi":1264},{"id":24,"text":1267,"url":24,"identifiers":1268},"10.1023\u002FA:1021886501912",{"doi":1267},{"id":24,"text":1270,"url":24,"identifiers":1271},"10.1023\u002FB:NARR.0000007804.27450.e8",{"doi":1270},{"id":24,"text":1273,"url":24,"identifiers":1274},"10.1080\u002F08120090500304257",{"doi":1273},{"id":24,"text":1276,"url":24,"identifiers":1277},"10.1071\u002FEG05401",{"doi":1276},{"id":24,"text":1279,"url":24,"identifiers":1280},"JICA‐MMAJ, 1994, Report on the Mineral Exploration in the Catanduanes Area, Phase I",{},{"id":24,"text":1282,"url":24,"identifiers":1283},"10.2113\u002F100.8.1583",{"doi":1282},{"id":24,"text":1285,"url":24,"identifiers":1286},"10.1016\u002Fj.oregeorev.2006.12.001",{"doi":1285},{"id":24,"text":1288,"url":24,"identifiers":1289},"Lewkowski C. Porwal A.andGonzález‐Álvarez I.(2010)Genetic programming applied to base‐metal prospectivity mapping in the Aravalli Province India. Geophysical Research Abstracts 12 EGU2010‐15171.",{},{"id":24,"text":1291,"url":24,"identifiers":1292},"10.1007\u002FBF01782267",{"doi":1291},{"id":24,"text":1294,"url":24,"identifiers":1295},"10.1007\u002FBF02286436",{"doi":1294},{"id":24,"text":1297,"url":24,"identifiers":1298},"10.1016\u002Fj.oregeorev.2010.02.004",{"doi":1297},{"id":24,"text":1300,"url":24,"identifiers":1301},"Mandelbrot B. B., 1983, The Fractal Geometry of Nature (updated and augmented edition)",{},{"id":24,"text":1303,"url":24,"identifiers":1304},"10.1088\u002F0031-8949\u002F32\u002F4\u002F001",{"doi":1303},{"id":24,"text":1306,"url":24,"identifiers":1307},"Miranda F. E.andVargas B. S.(1967)Geology and mineral resources of Catanduanes province. Philippine Bureau of Mines Report of Investigation No. 62 69p.",{},{"id":24,"text":1309,"url":24,"identifiers":1310},"10.1016\u002F0375-6742(90)90041-8",{"doi":1309},{"id":24,"text":1312,"url":24,"identifiers":1313},"Mitchell A. H. G., 1991, Epithermal Gold in the Philippines: Island Arc Metallogenesis, Geothermal Systems and Geology",{},{"id":24,"text":1315,"url":24,"identifiers":1316},"Mondlane S., 2006, Distribution patterns of gold deposits in the Archaean Manica–Mutare–Odzi greenstone belt, Gondwana Res., 707",{},{"id":24,"text":1318,"url":24,"identifiers":1319},"10.1111\u002Fj.1751-3928.2007.00041.x",{"doi":1318},{"id":24,"text":1321,"url":24,"identifiers":1322},"10.1007\u002Fs11053-008-9062-0",{"doi":1321},{"id":24,"text":1324,"url":24,"identifiers":1325},"10.1111\u002Fj.1751-3928.2008.00050.x",{"doi":1324},{"id":24,"text":1327,"url":24,"identifiers":1328},"Porwal A., 2006, Mineral Potential Mapping with Mathematical Geological Models",{},{"id":24,"text":1330,"url":24,"identifiers":1331},"10.1002\u002F9780470994559.ch9",{"doi":1330},{"id":24,"text":1333,"url":24,"identifiers":1334},"10.1023\u002FA:1025171803637",{"doi":1333},{"id":24,"text":1336,"url":24,"identifiers":1337},"10.1023\u002FB:MATG.0000041180.34176.65",{"doi":1336},{"id":24,"text":1339,"url":24,"identifiers":1340},"10.1016\u002Fj.cageo.2005.03.018",{"doi":1339},{"id":24,"text":1342,"url":24,"identifiers":1343},"10.1016\u002Fj.oregeorev.2005.10.003",{"doi":1342},{"id":24,"text":1345,"url":24,"identifiers":1346},"10.1016\u002Fj.oregeorev.2010.04.002",{"doi":1345},{"id":24,"text":1348,"url":24,"identifiers":1349},"Porwal A. Yu L.andGessner K.(2010b)SVM‐based base‐metal prospectivity modeling of the Aravalli Orogen northwestern India. Geophysical Research Abstracts 12 EGU2010‐15171.",{},{"id":24,"text":1351,"url":24,"identifiers":1352},"Raine M. D., 2004, Mining and Resource Geology Symposium: Proceedings Volume, 114",{},{"id":24,"text":1354,"url":24,"identifiers":1355},"10.1007\u002Fs11053-008-9067-8",{"doi":1354},{"id":24,"text":1357,"url":24,"identifiers":1358},"10.1023\u002FA:1021138910662",{"doi":1357},{"id":24,"text":1360,"url":24,"identifiers":1361},"10.1007\u002Fs11053-007-9042-9",{"doi":1360},{"id":24,"text":1363,"url":24,"identifiers":1364},"10.1023\u002FA:1012536823294",{"doi":1363},{"id":24,"text":1366,"url":24,"identifiers":1367},"10.1515\u002F9780691214696",{"doi":1366},{"id":24,"text":1369,"url":24,"identifiers":1370},"10.1016\u002FS0098-3004(01)00052-8",{"doi":1369},{"id":24,"text":1372,"url":24,"identifiers":1373},"10.1007\u002FBF02272804",{"doi":1372},{"id":24,"text":1375,"url":24,"identifiers":1376},"10.1007\u002Fs11004-007-9127-3",{"doi":1375},{"id":24,"text":1378,"url":24,"identifiers":1379},"10.1016\u002Fj.oregeorev.2010.02.001",{"doi":1378},{"id":24,"text":1381,"url":24,"identifiers":1382},"10.1007\u002FBF02068587",{"doi":1381},{"id":24,"text":1384,"url":24,"identifiers":1385},"10.1023\u002FA:1021606417010",{"doi":1384},{"id":24,"text":1387,"url":24,"identifiers":1388},"Singer D. A., 2001, Contributions to Global Mineral Resource Assessment Research. U.S, A1",{},{"id":24,"text":1390,"url":24,"identifiers":1391},"10.2113\u002F100.3.491",{"doi":1390},{"id":24,"text":1393,"url":24,"identifiers":1394},"10.1016\u002Fj.lithos.2004.03.008",{"doi":1393},{"id":24,"text":1396,"url":24,"identifiers":1397},"UNDP, 1987, Geochemical nature of epithermal gold mineralization and related anomalies in the Philippines",{},{"id":24,"text":1399,"url":24,"identifiers":1400},"10.2113\u002Fgsecongeo.94.4.475",{"doi":1399},{"id":24,"text":1402,"url":24,"identifiers":1403},"10.1016\u002FS0191-8141(01)00152-3",{"doi":1402},{"id":24,"text":1405,"url":24,"identifiers":1406},"10.1214\u002Faos\u002F1176350603",{"doi":1405},{"id":24,"text":1408,"url":24,"identifiers":1409},"10.1130\u002FG20475.1",{"doi":1408},{"id":24,"text":1411,"url":24,"identifiers":1412},"10.1016\u002Fj.jag.2009.07.001",{"doi":1411},{"id":24,"text":1414,"url":24,"identifiers":1415},"10.1016\u002Fj.oregeorev.2008.12.001",{"doi":1414},{"id":1417,"createTime":1418,"updateTime":1418,"relativeEntities":1419,"slug":1420,"properties":1421,"entityType":140,"verifyStatus":141,"verifyTime":1418,"verifyNote":142,"syncStatus":23,"languages":1433,"translateLanguages":24,"viewCount":25,"primaryUrl":1434,"fullTextUrl":24,"authors":1435,"publicationType":185,"publisherRelationship":1543,"citationCount":1580,"citationInfo":1581,"publishDate":1587,"publishYear":989,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1588,"isForceReanalyzing":663},"b33a9199-aed4-4b29-a807-565d74b3a29c","2024-10-16T02:01:45.558+00:00",[],"Paleozoic-Epithermal-Au-and-Porphyry-Cu-Deposits-in-North-Xinjiang-China-Epochs-Features-Tectonic-Linkage-and-Exploration-Significance",{"mag":1422,"keywords":1424,"openalex":1425,"abstract":1427,"title":1429,"doi":1431},{"VOID":1423},"2067546961",{},{"VOID":1426},"W2067546961",{"EN":1428},"\u003Cjats:p>\u003Cjats:bold>Abstract. \u003C\u002Fjats:bold> Based on field investigation of large number of ore deposits including some latest discoveries and multidiscipline comprehensive research, we demonstrated the general features of metallic deposits and we suggest that Paleozoic archipelago‐type collisional orogen at North Xinjiang, northwestern China show intimate similarity with the metallogenesis of Southeast Asia Cenozoic archipelago. We briefly described the characteristics of major porphyry‐type, skarn‐type Cu deposits and typical high‐sulfidation type (HS‐type) and low‐sulfidation type (LS‐type) epithermal Au deposits as well as some latest discoveries. Systematic isotopic age‐dating on the Tuwu‐Yandong superlarge porphyry Cu deposits revealed that they formed in Late Devonian to Early Carboniferous in an accretionary arc setting. The tectonic settings of epithermal Au deposits and its linkage with porphyry Cu deposits are further discussed. The formation condition for porphyry Cu deposits is more strict than epithermal Au deposits. The distribution width for porphyry Cu deposits in the orogenic belts is more limited than epithermal Au deposits. The discovery and prospecting progress of the Kalatage HS‐type Cu‐Au deposit were reported. The significance in further exploration was suggested.\u003C\u002Fjats:p>",{"EN":1430},"Paleozoic Epithermal Au and Porphyry Cu Deposits in North Xinjiang, China: Epochs, Features, Tectonic Linkage and Exploration 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