Sm-Nd and Rb-Sr isotopical ages of magnetite-chlorite formation gold deposit in the volcanic rock area of Late Paleozoic Era, East Tianshan |
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Authors: | Jinsheng Ji Huaqin Li Lianchang Zhang Xingke Yang Chengyou Feng |
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Affiliation: | (1) Xi’an Engineering University, 710054 Xi’an, China;(2) Yickang Institute of Geology and Mineral Resources, 443003 Yichang, China |
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Abstract: | Through studying geo-geochemical characteristics and determining Sm-Nd and Rb-Sr isotopical ages in the Kanggur magnetite-chlorite formation gold deposit, some conclusions can be achieved: Sm-Nd isochron age is (290.4 ± 7)Ma, Rb-Sr isochron age is (282.3 ± 5)Ma, mineralization is Late Hercynian and the formation of this gold deposit is related to the macroscopic Huangshan-Qiugemingtashi ductile shear zone which is produced as a result of collision between the Tarim plate and the Junggar plate. |
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Keywords: | gold deposit Sm-Nd isotope Rb-Sr isotope Kanggurtage |
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