The migration of Tarim plume magma toward the northeast in Early Permian and its significance for the exploration of PGE-Cu-Ni magmatic sulfide deposits in Xinjiang, NW China: As suggested by Sr-Nd-Hf isotopes, sedimentology and geophysical data
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- 作者：Yuegao Liua ; b ; Xinbiao Lü ; a ; c ; Chunming Wua ; wcmcug@cug.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Xiaoguang Huc ; Zhipeng Duanc ; Gang Dengd ; Heng Wangd ; Xikui Zhuc ; d ; Huadong Zengd ; Peng Wangd ; Wei Wangd ; Qiang Lud
- 关键词：Early Permian ; Mantle plume ; PGE-Cu&ndash ; Ni magmatic sulfide deposit ; Tarim
- 刊名：Ore Geology Reviews
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：72
- 期：part_P1
- 页码：538-545
- 全文大小：2243 K
文摘
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We inferred that the tendency of Tarim Early Permian mantle plume was southwest.
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Tarim plume magma possibly flowed toward the northeastern margin of the Tarim Basin.
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New Cu–Ni deposits in Early Permian may be found in the southwest area of Beishan.