西昆仑玛尔坎苏石炭纪大型锰矿带构造背景与成矿条件

doi:10.13278/j.cnki.jjuese.20190294

Abstract

Abstract: The large scale Carboniferous Malkansu manganese carbonate metallogenic belt in west Kunlun orogen is one of the most important prospecting achievement in China. The belt belongs to the back-arc extension basin of north Kunlun in Late Paleozoic. The basin was formed in the subduction of paleo Tethys Ocean beneath the Tarim plate. The Mn orebody is hosted by the marine sedimentary sequence of the Upper Carboniferous Kalaatehe Formation. The ore is composed of rhodochrosite (75%-95%), pyrolusite, alabandite, and pyrite. Based on petrographic and lithologic studies, it is suggested that the Upper Carboniferous Kalaratehe Formation represents sedimentary sequence of back-arc basin. Based on trace elements, C isotopes(δ¹³C=-23.3‰--10.0‰), it is suggested that the ore-forming condition of the Carboniferous Malkansu manganese ore body is normoxic . It is speculated that the dissimilatory reduction of manganese oxides in combination with organic matter resulted in the precipitation of manganese carbonates.

Key words: sedimentary manganese carbonate deposit, Carboniferous, tectonic setting, ore-forming condition, metallogenic model, Malkansu manganese ore belt, west Kunlun orogen

CLC Number:

P612

Zhang Lianchang, Zhang Banglu, Dong Zhiguo, Xie Yueqiao, Li Wenjun, Peng Zidong, Zhu Mingtian, Wang Changle. Tectonic Setting and Metallogenetic Conditions of Carboniferous Malkansu Giant Manganese Belt in West Kunlun Orogen[J].Journal of Jilin University(Earth Science Edition), 2020, 50(5): 1340-1357.

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Tectonic Setting and Metallogenetic Conditions of Carboniferous Malkansu Giant Manganese Belt in West Kunlun Orogen

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