The collision-type porphyry Mo deposits in Dabie Shan, China

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• 作者：Yan-Jing Chen^a ; ^b ; ^{yjchen@pku.edu.cn} ; ^{gigyjchen@126.com} ; Pin Wang^a ; Nuo Li^b ; Yong-Fei Yang^c ; Franco Pirajno^d
• 关键词：Collision-type porphyry Mo deposits ; Dabie Shan ; Continental collision ; Global tectonic model for porphyry Mo deposits ; Scissor-style intracontinental subduction model
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P2
• 页码：405-430
• 全文大小：5341 K
• 卷排序：81

文摘

Dabie Shan, China is a new Mo metallogenic belt with total reserve of > 3 Mt Mo Mineralization occurred in syn- to post-collision tectonic setting during 156–110 Ma Ores associate with high-K calc-alkaline granites sourced from continental crust A scissor-style A-type subduction model is proposed for the Dabie-Qinling area The Dabie porphyry Mo belt is of collision-type, instead of rift- or subduction-type