Discovery of coesite from Indus Suture Zone (ISZ), Ladakh, India: Evidence for deep subduction

Himanshu K. Sachani*, Barun K. Mukherjee, Yoshihide Ogasawara, Shigenori Maruyama, Haruhito Ishida, Atsumi Muko, Nobuhiro Yoshioka

*この研究の対応する著者

    研究成果: Article査読

    75 被引用数 (Scopus)

    抄録

    Coesite, the high-pressure polymorph of quartz has been identified for the first time in the Tso-Morari Crystalline Complex, Ladakh (India) in the Himalayan belt. The preservation of coesite grains as inclusions in garnet within eclogite boudins indicates the existence of UHP metamorphism in this continental collision setting. The coesite was identified optically and its presence confirmed by its characteristic Raman bands. Both coesite and polycrystalline quartz inclusions exhibit prominent radial fractures in their host garnet. The silica inclusions (monomineralic coesite, monomineralic quartz and bimineralic quartz+coesite) are associated with various textural features and well-developed chemical zonation within the garnet, which show the prograde nature of the UHP metamorphism. Preliminary P-T estimates suggest that the coesite growth took place at pressure > 28 kbar (> 90 km depth) and temperatures > 640°C. Significantly, the coesite inclusions are interpreted as having suffered decompression during exhumation without changing to quartz, most likely due to the rapid uplift. This finding also indicates deep subduction of the Indian plate beneath the Asian continent, The occurrence of coesite and subduction of the Indian plate was essentially governed by a low geothermal gradient which occurred prior to rapid exhumation. This was vital for generating the coherent picture of metamorphism and exposure of UHP rocks.

    本文言語English
    ページ(範囲)235-240
    ページ数6
    ジャーナルEuropean Journal of Mineralogy
    16
    2
    DOI
    出版ステータスPublished - 2004 3月

    ASJC Scopus subject areas

    • 地球化学および岩石学

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