REN Li-guo, WANG Xi-jun, XU Li-li, WANG Min, LIU Xi-zhong. GEOCHEMISTRY AND GENESIS OF THE ARCHEAN BANDED FERROSILICON FORMATION IN FUSHUN, LIAONING PROVINCE[J]. Geology and Resources, 2014, 23(1): 62-67. DOI: 10.13686/j.cnki.dzyzy.2014.01.009
    Citation: REN Li-guo, WANG Xi-jun, XU Li-li, WANG Min, LIU Xi-zhong. GEOCHEMISTRY AND GENESIS OF THE ARCHEAN BANDED FERROSILICON FORMATION IN FUSHUN, LIAONING PROVINCE[J]. Geology and Resources, 2014, 23(1): 62-67. DOI: 10.13686/j.cnki.dzyzy.2014.01.009

    GEOCHEMISTRY AND GENESIS OF THE ARCHEAN BANDED FERROSILICON FORMATION IN FUSHUN, LIAONING PROVINCE

    • The ore types and distribution of the Archean ferrosilicon formation in Fushun region is specifically related to the trans-Fushun Hunhe deep fault. Based on the characteristic of the ores in the ferrosilicon formation, the authors analyze the geochemistry of a few deposits, with the metallogenic background and process, to set up the ore-forming model of the Archean ferrosilicon formation in the region, i.e. the model of submarine volcanic exhalation/hot water-ore fluid submarine circulation-sedimentation-metamorphic recrystallization.
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