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ZHAO Hui, YANG JingSui, LIU Fei, XIONG Fahui, LIAN Dongyang, YAO Hu, DONG Yufei. 2019. Features of the Cuobuzha podiform chromitite along western Yarlung Zangbo suture zone in Tibet:Implications for its tectonic setting[J]. Geology in China, 46(1): 115-125. doi: 10.12029/gc20190107
Citation: ZHAO Hui, YANG JingSui, LIU Fei, XIONG Fahui, LIAN Dongyang, YAO Hu, DONG Yufei. 2019. Features of the Cuobuzha podiform chromitite along western Yarlung Zangbo suture zone in Tibet:Implications for its tectonic setting[J]. Geology in China, 46(1): 115-125. doi: 10.12029/gc20190107
shu

Features of the Cuobuzha podiform chromitite along western Yarlung Zangbo suture zone in Tibet:Implications for its tectonic setting

  • 1.

    Harbin Institute of Technology, Harbin 150001, Heilongjiang, China

  • 2.

    Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, Guangdong, China

  • 3.

    Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

  • 4.

    School of Earth Sciences and Engineering, Nanjing University, Nanjing 201123, Jiangsu, China

  • 5.

    Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China

    • Fund Project: Supported by Ministry of Science and Technology of China (No. 2014DFR21270), China Geological Survey (No. DD20160023-01 and DD20160022-01) and National Science Foundation of China (No. 41720104009, 41672063, 41773029)
More Information
  • Author Bio: ZHAO Hui, female, born in 1992, doctor candidate, majors in petrology; E-mail: 13717926721@163.com
  • Corresponding author: YANG Jingsui, male, born in 1950, academician of Chinese Academy of Sciences, majors in petrology and tectonics in Tibetan Plateau and orogenic belts; E-mail:yangjsui@163.com 
Received Date:  15 June 2018
Revised Date:  18 January 2019
Publish Date:  25 February 2019
    Abstract

  • Most of chromitite ores produced in China are from the Yarlung Zangbo ophiolite belt (YZSZ), which is divided into three parts:the eastern part (Qu Shui to Mo Tuo), the middle part (Ang Ren to Ren Bu) and the western part (Saga to the Sino-Indian border). Furthermore, the western part contains north sub-belt and south sub-belt. For a long time, most of studies have focused on the eastern part and middle part, with very insufficient studies conducted on the western part, especially on the north subbelt, which inhibits mineral exploration along the YZSZ. Cuobuzha ophiolite is located in the north sub-belt, which occurs along a NW-SE trending belt and is mainly composed of harzburgite with diabase dykes. The field investigation discovered several chromite orebodies 0.5-1 m long and 0.2-0.5 m thick within the ophiolite. All of the ores are massive. The analytical results by electron-probe micro-analyzer (EPMA) show that the Cuobuzha chromitite is of typical high-Cr variety with Cr number[Cr#=100×Cr/(Cr + Al)] ranging from 75 to 78, and Mg number[Mg#=100×Mg/(Mg + Fe2+)] ranging from 66 to 69. Calculated results show that the ratio of FeO/MgO ranges from 0.51 to 0.65, and that the values of Al2O3 and TiO2 are 11.27%-12.1% and 0.19%-0.4%, respectively, revealing that the Cuobuzha chromitite has boninitic affinities. However, the occurrence of clinopyroxene exsolution indicates that it should have experienced a deep process.

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