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    Volume 33 Issue 1
    Jan.  2008
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    ZHENG Jian-bin, CAO Zhi-min, AN Wei, 2008. Mineral Component, Texture and Forming Conditions of Hydrothermal Chimney on the East Pacific Rise 9°-10°N. Earth Science, 33(1): 19-25.
    Citation: ZHENG Jian-bin, CAO Zhi-min, AN Wei, 2008. Mineral Component, Texture and Forming Conditions of Hydrothermal Chimney on the East Pacific Rise 9°-10°N. Earth Science, 33(1): 19-25.

    Mineral Component, Texture and Forming Conditions of Hydrothermal Chimney on the East Pacific Rise 9°-10°N

    • Received Date: 2007-01-28
    • Publish Date: 2008-02-25
    • To characterize the hydrothermal processes of East Pacific rise at 9°-10°N, sulfide mineral compositions, textural and geochemical features of chimney ores were studied using ore microscope, scanning electron microscope, X-ray diffraction analysis, and electron microprobe techniques.Resultsshow that there are three mineral assemblages for the hydrothermal chimney ores, namely: (1) anhydrite + marcasite + pyrite, (2) pyrite + sphalerite + chalcopyrite, and (3) chalcopyrite + bornite + digenite + covellite. Mineral assemblages, zonational features, and geochemical characteristics of the ore minerals indicate that ore fluid temperature changed from low to high then to low with a maximum temperature up to 400 ℃. The chimney is a typical black smoker. The initial structure of the chimney was formed by the precipitation of anhydrites, and later the sulfides began to precipitate in the inner wall.

       

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