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Chen Duofu, Chen Guangqian, Chen Xianpei, Gao Jiyuan, Pan Jingming. Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 91-95.
Citation: Chen Duofu, Chen Guangqian, Chen Xianpei, Gao Jiyuan, Pan Jingming. Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 91-95.

Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province

  • Received Date: 1997-04-04
  • Bio-reef-chert Suite is an important rock assemblage for controlling Dajiangping superlarge pyrite deposits, Fankou super-large lead-zinc deposits and Changkeng superlarge gold-silver deposits. It is formed as a fixed and ordered suite at space andtime, rnmposed of carbonate rocks of reef facies, hydrothermal sedimentary rocks (ores), fine detrital rocks intercalated bandedmudlimestone, synchronous volcanic rocks, tuffaceous rocks and volcanic veins in the isostrata in mining area or in the neighbordistrict. It is also the comprehensive products of normal sedimentary process, biological process in basin, hydrothermal sedimentaryprows under basin base and magmatic process in the deep of lithosphere, when basin evoluted at a special stage in a special geologi-cal setting.
  • [1] 陈先沛.初论礁硅岩套-一种重要的含矿岩石组合.地球化学文集,中国科学院地球化学研究所编辑,北京:科学出版社,1986.37-44
    [2] 朱上庆,池三川.层控矿床及找矿‘北京:地质出版社,1992,1-194
    [3] 南颐.广东长坑金、银矿区斌矿地层及时代.广东地质,1993,(3):17-23
    [4] 杜均恩,施纯溪,陈楚湘.广东长坑金、银矿成矿特征.广东地质,1993,(3):1-8
    [5] 夏萍,张湖,王秀璋.粤西长坑金银矿区硅质岩成因的地球化学特征和成因探讨地球化学,1996,25(2):170-171.
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  • Received:  1997-04-04

Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province

Abstract: Bio-reef-chert Suite is an important rock assemblage for controlling Dajiangping superlarge pyrite deposits, Fankou super-large lead-zinc deposits and Changkeng superlarge gold-silver deposits. It is formed as a fixed and ordered suite at space andtime, rnmposed of carbonate rocks of reef facies, hydrothermal sedimentary rocks (ores), fine detrital rocks intercalated bandedmudlimestone, synchronous volcanic rocks, tuffaceous rocks and volcanic veins in the isostrata in mining area or in the neighbordistrict. It is also the comprehensive products of normal sedimentary process, biological process in basin, hydrothermal sedimentaryprows under basin base and magmatic process in the deep of lithosphere, when basin evoluted at a special stage in a special geologi-cal setting.

Chen Duofu, Chen Guangqian, Chen Xianpei, Gao Jiyuan, Pan Jingming. Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 91-95.
Citation: Chen Duofu, Chen Guangqian, Chen Xianpei, Gao Jiyuan, Pan Jingming. Ore-controlling Rock Assemblage of Hydrothermal Sedimentary Superlarge Ore Deposits Bio-Reef-Chert Suite, Guangdong Province[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 91-95.
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