Geology, geochronology and geochemistry of the Saishitang Cu deposit, East Kunlun Mountains, NW China: Constraints on ore genesis and tectonic setting
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- 作者：Hui Wanga ; Chengyou Fenga ; fengchy@cags.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Daxin Lia ; Chao Lib ; Tianzhu Dingc ; Fangzhou Liaoc
- 关键词：Zircon U&ndash ; Pb ; Molybdenite Re&ndash ; Os ; Geochemistry ; Ore genesis ; Tectonic setting ; Saishitang Cu deposit
- 刊名：Ore Geology Reviews
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：72
- 期：part_P1
- 页码：43-59
- 全文大小：3516 K
文摘
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Mineralization of Saishitang Cu deposit occurred in the Late Triassic (~ 222 Ma).
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The quartz diorite originated from lower crust with input of mantle components.
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The Saishitang porphyry–skarn mineral system is related to crust–mantle interaction.
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The Saishitang Cu deposit is formed in a post-collision environment.
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