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Compared with other large and supper-large porphyry copper deposits in China and the adjacent Cu-Au mineralized areas, the ore-forming processes and conditions were analyzed; and the possibility of forming large porphyry copper deposits in the Shaxi area was discussed. The present study indicated that the ore-forming fluid and material were mainly of magmatic origin, while meteoric water played a certain role in the ore-forming processes. Interactions between subducting and overriding plates provided a major driving force for the formation of igneous rocks and the deposition of metal elements in East China since Jurassic. Based on the geochemical data of the Shaxi intrusive, it is found that the copper (gold) mineralization is closely related to the genesis of adakite-like intrusive in the Shaxi area. This adakite-like intrusive was formed in the subduction environment as a result of the subduction of the West Pacific plate toward the East China continent, where there is a great potentiality to form a large porphyry copper deposit.",{"EN":120},"Formation of the adakite-like granitoid complex and porphyry copper-gold deposit in Shaxi from southern Tancheng-Lujiang fault belt: A clue to the West Pacific plate subduction",{"VOID":122},"[]",{"VOID":124},"Batchelor R.A. and Bowden P. (1985) Petrogenetic interpretation of granitoid rock series using multicationic parameters [J]. Chem. Geol. 48, 43–56.\nBureau of Geology and Mineral Resources of Anhui Province (1987) Regional Geology of Anhui Province (Geological Memoirs, SW.1, No. 5) [M]. pp.1–72l. Geological Publishing House, Beijing (in Chinese).\nChang Yinfo, Liu Xiangpei, and Wu Yianchang (1991) The Copper-Iron Belt of the Middle and Lower Reaches of the Changjiang River [M]. pp.1–379. 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Rev. 11, 229–248.\nZhang Qi, Wang Yan, and Wang Yuanlong (2001) Preliminary study on the components of the lower crust in east China Plateau during Yanshanian Period: Constraints on Sr and Nd isotopic compositions of adakite-like rocks [J]. Acta Petrologica Sinica. 17, 505–513 (in Chinese with English Abstract).\nZhou X.M. and Li W.X. (2000) Origin of Late Mesozoic igneous rocks in southeastern China: Implications for lithosphere subduction and underplating of mafic magmas [J]. Tectonophysics. 326, 269–287.\nZhou X.M., Sun T., Shen W.Z., Shu L.S., and Niu Y.L. (2006) Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: A response to tectonic evolution [J]. Episodes. 29, 26–33.\nZhou Zuoxia (1983) The characteristics of the porphyry copper deposits in China and their substances sources [J]. 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decomposition, temperatures of four organic Zn complexes were evaluated experimentally by determining the change in sphalerite solubility with temperature in aqueous solutions containing organic compounds. The results show that decomposition takes place at 180°±5°C for lactic acid-Zn complex, 200°±5°C for EDTA-Zn, 240°±5°C for quinone-Zn and 190°±5°C for fulvic acid-Zn. It is also shown that at 190°–200°C sphalerite solubility is 4 to 7 times higher in NaCl solution containing organic compounds than that in NaCl solution without organic compounds. Studies were also conducted on the contents of Pb and Zn complexed by fulvic acid and humic acid in aqueous solutions the infrared spectra of fulvic acid-Zn and humic acid-Zn complexes, the differential thermal analysis of fulvic acid, humic acid and quinone and EDTA, and the variation in fulvic acid solubility in the seawater with temperature.",{"EN":626},"Experimental studies of organic-Zn complexes and their stability",{"VOID":628},"[\"9371662855124187946\"]",{"VOID":630},"Laboratory of Organic Geochemistry and Sedimentology, «Organic Geochemistry», Science Press, Beijing, 1982, 282–296 (in Chinese).\nRashid, M. A. and J. D. Leonard,Chem. Geol., 11(1973), 89–97.\nPicard, G. L.,Geochem. et Cosmochem. Acta, 40(1976), 1347–1350.\nSholkovitz, E.R.,Geochem. et Cosmochem. Acta, 40(1976), 831–845.\nSholkovitz, E.R and Copland, D.,Geochem. et Cosmochem. Acta, 45(1981), 181–189.\nRashid, M.A. and L.H. King,Geochem. et Cosmochem. Acta, 34(1970), 193–201.\nBarnes, H.L.,Econ. Geol., 58(1963), 1054–1060.\nRashid, M.A.,Soil Science, 11(1971), 298–306.\nGiordano, T.H. and H.L. BarnesEcon. Geol., 76(1981), 2200–2211.\nRodder, E.,Econ. Geol. Mon., 3(1967), 349–362.\nRodder, E.,Econ. Geol. 66(1971), 777–781.\nFu Jiamo and Liu Dehan,Acta Sedimentologica Sinica, 4(1983), 15–28.\nCollins, A. G.,Geochemistry of Oil-waters, Elsevier Scientific Publishing Company, 1975, 212–219.\nNissenbaum, A., Baedecker, M. J. and I. R. Kaplan,Adv. in Org. Geochem., Pergamon Press, 1971, 427–440.\nNissenbaum, A. and D. J. Swaine,Geochem. et Cosmochem. Acta, 40(1976), 809–816.\nCollins, A. G.,Geochemistry of Oil-waters, Elsevier Scientific Publishing Company, 1975, 185.\nWilley, L. M., Kharaka, Y. K., Presser, T. S., Rapp, J. B. and I. Barnes,Geochem. et Cosmochem. Acta, 39(1975), 1707–1711.\nSverjensky, D. A.,Econ. Geol., 79(1984), 23–27.\nCarpenter, A. B., Trout, M. I. and E. E. Piekett,Econ. Geol. 69(1974), 1191–1206.\nFlaig, W.,Adv. in Org. Geochem., Pergamon Press, 1971, 427–440.\nSpiro, B. and Z. Aizenshtat,Adv. in Org. Geochem., John Willey, 1981, 799–807.\nLevesque, M. and M. Schnitzer,Soil Sci., 103(1967), 183–190.\nTu Guangchi et al., «Geochemistry of Chinese Strata-bound Deposits», Science Press, Beijing, 1(1984), 42–55. (in Chinese).\nBarnes, H.L. and Czamanske, G.K.,Geochemistry of Hydrothermal Ore Deposits, New York, Holt Rinehart and Wiston, 1967, 334–381.",{"VOID":632},"10.1007\u002FBF02866712","2024-06-26T14:15:56.985+00:00","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002FBF02866712",[636,651],{"id":637,"sortIndex":21,"researcher":20,"roles":638,"affiliations":639,"properties":648,"displayName":650,"givenName":20,"familyName":20},"79ec0376-228b-4823-8762-c9ef4e691155",[136],[640],{"id":641,"sortIndex":21,"affiliation":642,"properties":20},"83fd5997-703d-458d-8336-56b8579ace51",{"id":641,"createTime":20,"updateTime":20,"relativeEntities":643,"slug":20,"properties":644,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":647,"statistic":20},[],{"title":645},{"VI":646},"Institute of Geochemistry, Academia Sinica, China",[],{"title":649},{"VI":650},"Lu Jialan",{"id":652,"sortIndex":57,"researcher":20,"roles":653,"affiliations":654,"properties":661,"displayName":663,"givenName":20,"familyName":20},"8e117690-8a11-4c67-bf80-b493f47e540e",[136],[655],{"id":641,"sortIndex":21,"affiliation":656,"properties":20},{"id":641,"createTime":20,"updateTime":20,"relativeEntities":657,"slug":20,"properties":658,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":660,"statistic":20},[],{"title":659},{"VI":646},[],{"title":662},{"VI":663},"Yuan Ziqiang",{"url":634,"publisher":665,"properties":679},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":666,"slug":10,"properties":667,"entityType":18,"verifyStatus":19,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":21,"subjectFields":671,"manageAffiliations":672,"indexDatabases":673,"url":20,"thumbnailPath":20,"statistic":674,"gsStatistic":20,"type":20,"analyzePriority":20},[],{"issn":668,"title":669,"eissn":670},{"VOID":13},{"EN":15},{"VOID":17},[],[],[],{"impactFactor":21,"impactFactorByYear":675,"i10Index":32,"i10IndexLast5Year":21,"totalPublication":33,"totalPublicationByYear":676,"totalCitation":55,"totalCitationByYear":677,"totalCitationPerPublication":76,"totalCitationPerPublicationByYear":678,"hindexLast5Year":105,"hindex":105},{"2012":27,"2013":28,"2014":29,"2015":30,"2016":29,"2017":31},{"1982":35,"1983":36,"1984":37,"1985":38,"1986":38,"1987":39,"1988":38,"1989":40,"1990":37,"1991":40,"1992":38,"1993":41,"1994":41,"1995":38,"1996":41,"1997":37,"1998":42,"1999":32,"2000":39,"2001":37,"2002":43,"2003":44,"2004":42,"2005":45,"2006":46,"2007":47,"2008":48,"2009":49,"2010":50,"2011":51,"2012":52,"2013":47,"2014":53,"2015":54},{"1982":53,"1983":57,"1984":58,"1985":54,"1986":59,"1987":60,"1988":61,"1989":62,"1990":63,"1991":64,"1992":32,"1993":65,"1994":66,"1995":36,"1996":67,"1997":43,"1998":39,"1999":68,"2000":57,"2001":69,"2002":70,"2003":61,"2004":63,"2005":39,"2006":71,"2007":72,"2008":53,"2009":43,"2010":72,"2011":73,"2012":74,"2013":52,"2014":75,"2015":43},{"1982":78,"1983":29,"1984":79,"1985":80,"1986":27,"1987":81,"1988":82,"1989":83,"1990":84,"1991":85,"1992":86,"1993":87,"1994":88,"1995":76,"1996":89,"1997":90,"1998":91,"1999":92,"2000":29,"2001":93,"2002":94,"2003":95,"2004":96,"2005":97,"2006":98,"2007":99,"2008":100,"2009":88,"2010":101,"2011":102,"2012":86,"2013":103,"2014":104,"2015":89},{"pages":680,"volume":682},{"VOID":681},"369-380",{"VOID":683},"5",{"total":61,"publishYear":685,"statisticByYear":686},1986,{},"1986-10-01","DONE_ANALYZE_CITATION","2026-07-19T09:07:10.248+00:00",[],{"id":692,"createTime":693,"updateTime":694,"relativeEntities":695,"slug":696,"properties":697,"entityType":127,"verifyStatus":128,"verifyTime":706,"verifyNote":130,"languages":20,"translateLanguages":20,"viewCount":21,"primaryUrl":707,"fullTextUrl":20,"authors":708,"publicationType":200,"publisherRelationship":763,"citationCount":59,"citationInfo":783,"publishDate":786,"publishYear":784,"citationAnalyzeStatus":19,"lastCitationAnalyze":787,"indexDatabases":788,"openAccess":20,"references":789,"isForceReanalyzing":225},"5ab3eca5-b4c6-492b-803a-374c20efdd79","2023-12-26T05:27:41.072+00:00","2026-05-06T16:23:49.016+00:00",[],"The-Silurian-reservoir-bed-differentiated-asphalts-in-Tarim-Basin-and-modeling-experiments-on-their-origin",{"abstract":698,"title":700,"gsPaper":702,"doi":704},{"EN":699},"There is a type of asphalt that originated from differentiation from reservoir bed (named reservoir bed-differentiated asphalt) in the Silurian asphaltic sandstones of the Tarim Basin. These asphalts are the result of second-time charging of hydrocarbons into the Silurian reservoir, which were derived from Lower Paleozoic source rocks. Asphalt was differentiated from the reservoir bed in the hydrocarbon gathering area of secondary migration. The differentiation is caused by changes in reservoir physical properties when pearl or chain hydrocarbons migrating through and gathering in the reservoir bed, and light components are lost and heavy ones are involved in the formation of asphalt or heavy oil. There are two kinds of occurrence of these asphalts in the Silurian system of the Tarim Basin. One is the poor heavy oil layer with lower oil saturation in trap and the other is scattered hydrocarbon distributed along the transport layer and unconformity surface. Reservoir bed-differentiated asphalts have two characteristics: total hydrocarbon content is high in extractable organic matter and the ratio of saturated to aromatic hydrocarbon is usually greater than unity. The physically modeling experiment has confirmed these characteristics and the genesis of the reservoir bed-differentiated asphalts.",{"EN":701},"The Silurian reservoir bed-differentiated asphalts in Tarim Basin and modeling experiments on their origin",{"VOID":703},"[\"10768862066332388133\"]",{"VOID":705},"10.1007\u002FBF02831085","2024-05-02T04:45:51.749+00:00","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002FBF02831085",[709,724,737,750],{"id":710,"sortIndex":21,"researcher":20,"roles":711,"affiliations":712,"properties":721,"displayName":723,"givenName":20,"familyName":20},"8c5bf04a-fd91-413e-b99d-98c1394be0f3",[136],[713],{"id":714,"sortIndex":21,"affiliation":715,"properties":20},"dbafdab9-88e0-4dba-841a-33076fa37e7b",{"id":714,"createTime":20,"updateTime":20,"relativeEntities":716,"slug":20,"properties":717,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":720,"statistic":20},[],{"title":718},{"VI":719},"University of Petroleum, Changping, Beijing, China",[],{"title":722},{"VI":723},"Liu 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Hongjiang",{"id":738,"sortIndex":59,"researcher":20,"roles":739,"affiliations":740,"properties":747,"displayName":749,"givenName":20,"familyName":20},"a0c74b6f-7464-4ea9-ac60-dc6516892ea5",[136],[741],{"id":714,"sortIndex":21,"affiliation":742,"properties":20},{"id":714,"createTime":20,"updateTime":20,"relativeEntities":743,"slug":20,"properties":744,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":746,"statistic":20},[],{"title":745},{"VI":719},[],{"title":748},{"VI":749},"Wang Hongyu",{"id":751,"sortIndex":188,"researcher":20,"roles":752,"affiliations":753,"properties":760,"displayName":762,"givenName":20,"familyName":20},"e681a113-770e-441e-a632-aa23db2d970c",[136],[754],{"id":714,"sortIndex":21,"affiliation":755,"properties":20},{"id":714,"createTime":20,"updateTime":20,"relativeEntities":756,"slug":20,"properties":757,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":759,"statistic":20},[],{"title":758},{"VI":719},[],{"title":761},{"VI":762},"Zeng 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Guochen and Zhang Yiwei, 1999, A study on the evolution of reservoirs in the Tarim Basin in the view of Earth’s crust wave movement [J]: Acta Petrolei Sinica, v.20, n.2, p. 7–11 (in Chinese).",{},{"id":20,"text":794,"url":20,"identifiers":795},"Liu Luofu, Zhao Jianzhang, Zhang Shuichang, Fang Jiahu, and Xiao Zhongyao, 2000a, Hydrocarbon filling ages and evolution of the Silurian asphalt sandstones in the Tarim Basin [J]: Acta Sedimentologica Sinica, v. 18, n. 3, p. 475–479 (in Chinese).",{},{"id":20,"text":797,"url":20,"identifiers":798},"Liu Luofu, Zhao Jianzhang, Zhang Shuichang, Fang Jiahu, and Xiao Zhongyao, 2000b, Genetic types and characteristics of the Silurian asphaltic sandstones in the Tarim Basin [J]: Acta Petrolei Sinica, v.21, n.6, p.12–17 (in Chinese).",{},{"id":20,"text":800,"url":20,"identifiers":801},"Liu Luofu, Fang Jiahu, and Wang Hongyan, 2001, Petrological characteristics of the Silurian asphaltic sandstones in the Tarim Basin and the significance of studying them [J]: Journal of Xi’an Petroleum Institute, v. 16, n. 1, p. 16–22 (in Chinese).",{},{"id":20,"text":803,"url":20,"identifiers":804},"Lu Xiuxiang, Zhang Yiwei, and Jin Zhijun, 1997, Genesis of the Silurian asphalt sandstones in the Tazhong uplift of the Tarim Basin, NW China [J]: Scientia Geologica Sinica, v.6, n.4, p.449–455.",{},{"id":806,"createTime":807,"updateTime":808,"relativeEntities":809,"slug":810,"properties":811,"entityType":127,"verifyStatus":128,"verifyTime":824,"verifyNote":130,"languages":20,"translateLanguages":825,"viewCount":21,"primaryUrl":827,"fullTextUrl":20,"authors":828,"publicationType":200,"publisherRelationship":892,"citationCount":911,"citationInfo":912,"publishDate":914,"publishYear":784,"citationAnalyzeStatus":19,"lastCitationAnalyze":915,"indexDatabases":916,"openAccess":20,"references":917,"isForceReanalyzing":225},"db55293c-091a-4feb-800e-22df4f69ddfc","2024-02-05T12:56:18.591+00:00","2026-04-09T11:22:47.465+00:00",[],"The-correlation-of-inorganic-C-O-isotopic-values-for-Lake-Chenghai-sediments-and-its-environmental-implications",{"abstract":812,"title":815,"gsPaper":818,"keywords":820,"doi":822},{"VI":813,"EN":814},"Là một trong những hồ trên cao nguyên Vân Nam-Quý Châu, hồ Chenghai là một hồ kín điển hình với lượng mưa chiếm khoảng một phần ba hoặc hơn của tổng nước đầu vào hàng năm, có độ mặn tổng thể cao (gần như giống với một hồ nước mặn). Thành phần đồng vị C, O vô cơ của trầm tích hồ mang nhiều thông tin nhạy cảm về sự biến đổi môi trường trong vùng lưu vực, trong khi mối tương quan của chúng tiết lộ những điều kiện thuỷ văn mà hồ đã bị khép kín. Sự biến đổi thành phần của chúng bị kiểm soát bởi nhiệt độ, lượng mưa, quang hợp, trạng thái cân bằng phân giải của hệ thống cacbonat và điều kiện thuỷ văn. Theo nghiên cứu của chúng tôi về thành phần đồng vị C, O vô cơ của trầm tích hồ Chenghai, chúng tôi đã khảo sát sự biến đổi môi trường của vùng lưu vực này từ vài thập kỷ trước. Kết quả cho thấy hồ Chenghai đã duy trì điều kiện thuỷ văn đóng kín tốt trong vài thập kỷ qua, như được chỉ ra bởi mối tương quan tốt của thành phần đồng vị C, O vô cơ của trầm tích; và sự biến đổi môi trường trong vùng lưu vực này có xu hướng tiến hóa theo chu kỳ trên thang thời gian 10−11 năm, mặc dù tiếng ồn tín hiệu tương đối cao ở đáy lõi trầm tích. Chúng tôi cũng có thể mở rộng việc sử dụng đồng vị C, O, một chỉ số môi trường nhạy cảm, cho đến các môi trường hồ gần như mặn với mức độ khoáng hóa cao.","As one of the lakes on the Yunnan-Guizhou plateau, Lake Chenghai, which is a typical closed lake with the precipitation accounting for one-third or more of the annual water input, has a high total salinity (almost like a saline lake). The inorganic C, O isotopic composition of lake sediments bears much sensitive information about environmental change in the catchment, while their correlations revealed the hydrological conditions under which the lake was closed. Their compositional variations are controlled by temperature, precipitation, photosynthesis, dissolving equilibrium of the carbonate system and hydrological condition. According to our research on inorganic C, O isotopic composition of Lake Chenghai sediments, we investigated the environmental change of this catchment several decades ago. The results showed that Lake Chenghai has kept good hydrological closing conditions in the past several decades, as indicated by the good correlation of inorganic C, O isotopic composition of sediments; and that the environmental change in this catchment shows a tendency of periodical evolution on a 10−11-years scale, although the signal noise is relatively high at the bottom of the sediment core. And we also can extend C, O isotopes, a sensitive environmental indicator, to nearly saline lake environments with a high degree of mineralization.",{"EN":816,"VI":817},"The correlation of inorganic C, O isotopic values for Lake Chenghai sediments and its environmental implications","Sự tương quan của các giá trị đồng vị C, O vô cơ trong trầm tích hồ Chenghai và những tác động môi trường của nó",{"VOID":819},"[\"1303801412894301274\"]",{"VI":821},"hồ Chenghai, đồng vị C, O, biến đổi môi trường, thuỷ văn, trầm tích 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In addition, intensive studies on inclusion characteristics of natural gems could identify their geographical origins and provide valuable information on gem synthesis. In this paper synthetic gems (synthetic star-spangled sapphire and emerald) and natural gems from various locations including natural sapphire from Thailand and Australia, and natural aquamerine from Mufushan, Hunan Province, and Ailaoshan, Yunnan Province, were selected for the comparative study of inclusions. Significant research results have been achieved, thus providing the important basis for distinguishing natural from synthetic gems.",{"EN":1173},"Study on inclusions in natural and synthetic gems",{"VOID":1175},"[\"10718664797527470815\"]",{"VOID":1177},"10.1007\u002FBF03166857","2024-05-01T10:34:41.485+00:00","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002FBF03166857",[1181],{"id":1182,"sortIndex":21,"researcher":20,"roles":1183,"affiliations":1184,"properties":1193,"displayName":1195,"givenName":20,"familyName":20},"01e4de2a-5656-4948-9050-2503b26834ff",[136],[1185],{"id":1186,"sortIndex":21,"affiliation":1187,"properties":20},"b31e83a8-e0a4-42d4-9363-62d2ec2c1b85",{"id":1186,"createTime":20,"updateTime":20,"relativeEntities":1188,"slug":20,"properties":1189,"entityType":20,"verifyStatus":20,"verifyTime":20,"verifyNote":20,"languages":20,"translateLanguages":20,"viewCount":20,"url":20,"parentIds":1192,"statistic":20},[],{"title":1190},{"VI":1191},"Department of 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Zhaolin (chief editor), 1988, Experimental geochemistry: Beijing, Geological Publishing House, p.209–224 (in Chinese).",{},{"id":20,"text":1226,"url":20,"identifiers":1227},"Li Zhaolin, Mao Yanhua, Lei Lihong, Qiu Zhili, and Niu Hecai, 1994, Physicochemical conditions of formation of beryl and quamarine in Mufushan granopegmatite deposit, Hunan Province, China: Chinese Journal of Geochemistry, v. 13, n. 4, p. 326–339.",{},{"id":20,"text":1229,"url":20,"identifiers":1230},"Li Zhaolin and Li Wen, 1995, Application of mineral inclusions in the study of gem mineral materials, in Peng Mingsheng and Zhang Huifen, eds., Mineral physics and mineral materials new technology: Guangzhou, Zhongshan University Publishing House, p. 153–156 (in Chinese).",{},{"id":20,"text":1232,"url":20,"identifiers":1233},"Li Zhaolin, Li Wen, Yang Rongyong, and Zhai Wei, 1998, The physical and chemical conditions for the formation and genesis of the Yakou gem pegmatite in the Ailaoshan metamorphic belt: Mineral Deposits, v. 17(sup.), p.453–456 (in Chinese with English abstract).",{},{"id":20,"text":1235,"url":20,"identifiers":1236},"Li Zhaolin, Yang Rongyong, Li Wen, Zhai Wei, and Mao Yanhua, 1998, Study on the physical and chemical conditions for the formation of different genetic types of pegmatite in China: Geological Science and Technology Information, v. 17, n. 72, p. 29 -34 (in Chinese with English abstract).",{},{"id":922,"text":1238,"url":924,"identifiers":1239},"Li Zhaolin, Yang Rongyong, and Li Wen, 1999, Pegmatite fluids of different origins and their implications for mineralization: Chinese Journal of Geochemistry, v. 18, n. 1, p. 9–17.",{"doi":926},{"id":20,"text":1241,"url":20,"identifiers":1242},"Li Zhaoling, Li Wen, and Zhai Wei, 1999, Crystalline fluid-melt inclusions in aquamarines in pegmatite of different origins: Chinese Science Bulletin, v.44 (sup. 2, Low-temperature geochemistry), p. 154–156.",{},{"id":20,"text":1244,"url":20,"identifiers":1245},"Li Zhaolin, Zhang Wenlan, Yang Rongyong, Li Wen, and Zhai Wei, 1999, Analysis of melt inclusion of chemical composition of beryl in pegmatite and discovery of zincpinel by electron probe: Chinese Science Bulletin, v. 44, n.21, p.2004–2009.",{},{"id":20,"text":1247,"url":20,"identifiers":1248},"Roedder, E., 1986, Fluid inclusions: Mineralogical Society of America, p. 48–58.",{},{"id":922,"text":1250,"url":924,"identifiers":1251},"Shepherd, T.J., A. H. Renkin, and D.H.M. Alderton, 1990, Practical guide to fluid inclusion studies: Wuhan, China University of Geology Publishing House ( Chinese version, translated by Zhang Enshi, Zhang Wenhuai, Gao Huaizhong, and Wang Siyuan), p.22–34.",{"doi":926},{"id":20,"text":1253,"url":20,"identifiers":1254},"Zeng Yiliang, Chen Changsheng, and Song Chengliang, 1994, Experimental study on the synthesis technology of emerald: Bulletin of Mineralogy, Petrology and Geochemistry, n.1, p.9-11 (in Chinese).",{}]