BIAN Xiong-fei. THE NARIGONGMA PORPHYRY MOLYBDENUM(-COPPER) DEPOSIT IN QINGHAI PROVINCE: Alteration[J]. Geology and Resources, 2012, 21(4): 390-394. DOI: 10.13686/j.cnki.dzyzy.2012.04.012
    Citation: BIAN Xiong-fei. THE NARIGONGMA PORPHYRY MOLYBDENUM(-COPPER) DEPOSIT IN QINGHAI PROVINCE: Alteration[J]. Geology and Resources, 2012, 21(4): 390-394. DOI: 10.13686/j.cnki.dzyzy.2012.04.012

    THE NARIGONGMA PORPHYRY MOLYBDENUM(-COPPER) DEPOSIT IN QINGHAI PROVINCE: Alteration

    • The Narigongma porphyry molybdenum (-copper) deposit in Southern Qinghai Province is located in the northern part of Yulong metallogenic belt. Research on the deposit recognizes three types of alteration in the orefield, i.e. K-silicate alteration (biotite-K feldspar), propylitic alteration (chlorite-epidote±calcite) and feldspar-destructive alteration (sericite±kaolin±calcite±anhydrite). The metallogenesis is closely related to the quartz-molybdenite±anhydrite±chalcopyrite±pyrite vein and molybdenite±pyrite±chalcopyrite vein.
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