Origin of the Badaguan porphyry CuMo deposit, Inner Mongolia, northeast China: Constraints from geology, isotope geochemistry and geochronology

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• 作者：Kuifeng Mi ; Zhenjiang Liu ; ^{lzj@cugb.edu.cn} ; Chunfeng Li ; Ruibin Liu ; Jianping Wang ; Runmin Peng
• 关键词：Mongol&ndash ; Okhotsk suture belt ; Erguna Block ; Badaguan porphyry CuMo deposit ; SrNdHf isotopes ; HOSPb isotopes
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P1
• 页码：154-172
• 全文大小：4122 K
• 卷排序：81

文摘

The magmatic rocks are generated from the partial melting of juvenile lower crust. HO and SPb isotopic data suggests magma–related fluid source. The deposit formed during subduction of Mongol–Okhotsk plate beneath the Erguna Block.