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2021 Vol. 48, No. 2
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WANG Zhaolin, MENG Guixiang, TANG Hejun, YUAN Lulu, YANG Zhusen, XIAO Yandong. 2021. Geochemistry of clinopyroxene and chrome spinel in the Zhaheba peridotite, Eastern Junggar, Xinjiang, China and its chromitite metallogenesis[J]. Geology in China, 48(2): 477-494. doi: 10.12029/gc20210209
Citation: WANG Zhaolin, MENG Guixiang, TANG Hejun, YUAN Lulu, YANG Zhusen, XIAO Yandong. 2021. Geochemistry of clinopyroxene and chrome spinel in the Zhaheba peridotite, Eastern Junggar, Xinjiang, China and its chromitite metallogenesis[J]. Geology in China, 48(2): 477-494. doi: 10.12029/gc20210209
shu

Geochemistry of clinopyroxene and chrome spinel in the Zhaheba peridotite, Eastern Junggar, Xinjiang, China and its chromitite metallogenesis

  • 1.

    Chinese Academy of Geological Sciences, Beijing, 100037, China

  • 2.

    SinoProbe Center, Chinese Academy of Geological Sciences and China Geological Survey, Beijing, 100037, China

  • 3.

    Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037, China

  • 4.

    Geological Research Academy of Xinjiang, Urimqi, 830000, Xinjiang, China

    • Fund Project: Supported by the project of China Geological Survey (No. DD20190071) and scientific research project of Chinese Academy of Geological Sciences (No. JKY201908-01)
More Information
  • Author Bio: WANG Zhaolin, male, born in 1978, senior engineer, engaged in metal mineral exploration and research; Email: geology231@126.com
Received Date:  04 December 2019
Revised Date:  18 February 2020
Publish Date:  25 April 2021
    Abstract

  • Zhaheba ophiolite is a significant ophiolite complex in Eastern Junggar, consisting mainly of peridiotite, basalt, layered gabbro, plagiogranite and chert. Among them, the peridiotite is mainly composed of harzburgite, herzolite, and minor dunite. The average contents of clinopyroxene in herzolite are Cr2O3 1.11%, Al2O3 4.77%, MgO 16.99%, CaO 21.84%, SiO2 50.00%, and the accessory mineral chromium spinel falling within the high-Al types has lower average contents Cr2O3 40.35%、Cr# 0.53 but higher Al2O3 24.10%, MgO 13.23% and Mg#(0.62), which indicate that it was formed during the extension of Zhaheba ocean in MOR environment. While the element contents of chrome spinels in massive chromites changes little with average contents of Cr2O3 55.45%、Al2O3 10.88%, MgO 11.98% and Mg# 0.60, which fall in high-Cr type fields and belong to SSZ type of chromites. Clinopyroxenes in herzolite is characterized by typical structures of melted residue and melt-rock reaction, and orthopyroxene in harzburgite kept bastitic pseudomorphs and unaltered enstatites, but chrome spinel accessory minerals show corrosion features. The melting residual structure of monocline is a manifestation of the melting and chromium release of chromium-bearing minerals, and also a structural indicator of the partial melting degree of peridotite increasing and the evolution towards more magnesium rich direction, which may have limited contribution to the formation of Cr-rich chromite. The peridotite contains monoclinopyroxene, olivine and textures newly generated from melt-rock reaction. The role of fluid and volatiles in the melt-rock reaction cannot be ignored. Based on the above studies, the relationship among the content differences of Cr#、Mg# and Al2O3 of chromite and tectonic settings of ophiolite, and its influence factors are discussed. It is concluded that mantle convection and subduction of Kalamaili ocean led to the enrichment of the high-Al chrome spinels in MOR environment and forming of massive chromites.

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