Isotopic indication to source of ore materials and fluids of the Wangfeng gold deposit in Tianshan: A case study of metallogenesis during collisional orogenesis
The Wangfeng gold deposit is one of the five most important gold deposits in the Tianshan. Studies of its metallogenic time, space, geodynamic background, ore feature and ore fluid have proved that the deposit formed in the late Paleozoic continental collision, and consequently is a suitable delegat...
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| Veröffentlicht in: | Science China. Earth sciences 2000-12, Vol.43 (S1), p.156-166 |
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| creator | Chen, Huayong Bao, Jingxin Zhang, Zengjie Liu, Yulin Ni, Pei Ling, Hongfei |
| description | The Wangfeng gold deposit is one of the five most important gold deposits in the Tianshan. Studies of its metallogenic time, space, geodynamic background, ore feature and ore fluid have proved that the deposit formed in the late Paleozoic continental collision, and consequently is a suitable delegate to probe mineralizing regularities during collisional orogenesis. Isotopic studies including O, D, C, S, Pb and Sr reveal ore materials derived from sedimentary association (including carbonate and sulfate), which further refers to the Hercynian carbonate-silicolite-argillite formation north to Wangfeng camp. At the end of Paleozoic, the southward intracontinental subduction of Hercynian synthem along the Hongwuyueqiao fault down to the Central Tianshan terrane induced large-scale fluidization which extracted and out-transported ore materials from Hercynian synthem upto shallow fair positions, and finally resulted in the formation of the Wangfeng deposit. This study excludes the possibility of other tectonic metallogenic models other than the tectonic model for collisional metallogenesis, petrogenesis and fluidization. |
| doi_str_mv | 10.1007/BF02911941 |
| format | Article |
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Studies of its metallogenic time, space, geodynamic background, ore feature and ore fluid have proved that the deposit formed in the late Paleozoic continental collision, and consequently is a suitable delegate to probe mineralizing regularities during collisional orogenesis. Isotopic studies including O, D, C, S, Pb and Sr reveal ore materials derived from sedimentary association (including carbonate and sulfate), which further refers to the Hercynian carbonate-silicolite-argillite formation north to Wangfeng camp. At the end of Paleozoic, the southward intracontinental subduction of Hercynian synthem along the Hongwuyueqiao fault down to the Central Tianshan terrane induced large-scale fluidization which extracted and out-transported ore materials from Hercynian synthem upto shallow fair positions, and finally resulted in the formation of the Wangfeng deposit. This study excludes the possibility of other tectonic metallogenic models other than the tectonic model for collisional metallogenesis, petrogenesis and fluidization.</description><identifier>ISSN: 1006-9313</identifier><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1862-2801</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1007/BF02911941</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Carbonates ; Computational fluid dynamics ; Deposits ; Fluid flow ; Fluidization ; Fluidizing ; Fluids ; Gold ; Metallogenesis ; Mineral deposits ; Paleozoic ; Petrogenesis ; Plate tectonics ; Subduction ; Subduction (geology) ; Sulfates ; Tectonics</subject><ispartof>Science China. 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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Huayong</au><au>Bao, Jingxin</au><au>Zhang, Zengjie</au><au>Liu, Yulin</au><au>Ni, Pei</au><au>Ling, Hongfei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Isotopic indication to source of ore materials and fluids of the Wangfeng gold deposit in Tianshan: A case study of metallogenesis during collisional orogenesis</atitle><jtitle>Science China. Earth sciences</jtitle><date>2000-12-01</date><risdate>2000</risdate><volume>43</volume><issue>S1</issue><spage>156</spage><epage>166</epage><pages>156-166</pages><issn>1006-9313</issn><issn>1674-7313</issn><eissn>1862-2801</eissn><eissn>1869-1897</eissn><abstract>The Wangfeng gold deposit is one of the five most important gold deposits in the Tianshan. Studies of its metallogenic time, space, geodynamic background, ore feature and ore fluid have proved that the deposit formed in the late Paleozoic continental collision, and consequently is a suitable delegate to probe mineralizing regularities during collisional orogenesis. Isotopic studies including O, D, C, S, Pb and Sr reveal ore materials derived from sedimentary association (including carbonate and sulfate), which further refers to the Hercynian carbonate-silicolite-argillite formation north to Wangfeng camp. At the end of Paleozoic, the southward intracontinental subduction of Hercynian synthem along the Hongwuyueqiao fault down to the Central Tianshan terrane induced large-scale fluidization which extracted and out-transported ore materials from Hercynian synthem upto shallow fair positions, and finally resulted in the formation of the Wangfeng deposit. This study excludes the possibility of other tectonic metallogenic models other than the tectonic model for collisional metallogenesis, petrogenesis and fluidization.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1007/BF02911941</doi><tpages>11</tpages></addata></record> |
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| ispartof | Science China. Earth sciences, 2000-12, Vol.43 (S1), p.156-166 |
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| subjects | Carbonates Computational fluid dynamics Deposits Fluid flow Fluidization Fluidizing Fluids Gold Metallogenesis Mineral deposits Paleozoic Petrogenesis Plate tectonics Subduction Subduction (geology) Sulfates Tectonics |
| title | Isotopic indication to source of ore materials and fluids of the Wangfeng gold deposit in Tianshan: A case study of metallogenesis during collisional orogenesis |
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