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Article Navigation >  Acta Sedimentologica Sinica  > 1984  >  2(3): 34-47

Chen Yaoqin, Zeng Bofu. GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG[J]. Acta Sedimentologica Sinica, 1984, 2(3): 34-47.
Citation: Chen Yaoqin, Zeng Bofu. GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG[J]. Acta Sedimentologica Sinica, 1984, 2(3): 34-47.
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GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG

  • Nichang Institute of Geology and Mineral Resources, Ministry of Geology and Mineral Resources

  • Received Date: 1982-12-16
  • Publish Date: 1984-09-10
  • The huge lead and zinc deposit of Fankou, Guangdong is a strata-bound ore deposit located in carbonate rocks of Middle -Upper Devonian series. The orebody chiefly appears in the transition zone between the carbonate rock and the fragme-ntal rock, and also in the carbonate rock. The orebody is controlled by faults.The ore-bearing rocks mostly are micrites with a great deal of algaes and contain a good few of terrigenous clastic and carbonaceous sediments. The dolomitization of the ore-bearing rocks is not intense. There are, however, residues of wall rocks in the orebody which is bordered by joints on the surrounding rock.
  • [1] (1)中国科学院地球化学研究所有机地球化学研究室，198:3，有机地球化学，科学出版社.

    (2)刘宝裙主编1980,沉积岩石学、地质出版社.

    (3)王英华等，1983,氧、碳同位素组成在研究碳酸盐岩成宕作用中的意义，地质评论、29卷第3期。

    (4)H. Skall，1975, The paleoewironment of the Pine Point Lead-Zine District,ECONOMIC GEOLOGY 1973.N0.1.
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  • Received:  1982-12-16
  • Published:  1984-09-10

GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG

  • Nichang Institute of Geology and Mineral Resources, Ministry of Geology and Mineral Resources
  • Received Date: 1982-12-16
  • Publish Date: 1984-09-10

Abstract: The huge lead and zinc deposit of Fankou, Guangdong is a strata-bound ore deposit located in carbonate rocks of Middle -Upper Devonian series. The orebody chiefly appears in the transition zone between the carbonate rock and the fragme-ntal rock, and also in the carbonate rock. The orebody is controlled by faults.The ore-bearing rocks mostly are micrites with a great deal of algaes and contain a good few of terrigenous clastic and carbonaceous sediments. The dolomitization of the ore-bearing rocks is not intense. There are, however, residues of wall rocks in the orebody which is bordered by joints on the surrounding rock.

Chen Yaoqin, Zeng Bofu. GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG[J]. Acta Sedimentologica Sinica, 1984, 2(3): 34-47.
Citation: Chen Yaoqin, Zeng Bofu. GEOLOGIC CHARACTERISTICS AND GENESIS OF HUGE STRATA-BOUND LEAD-ZINC ORE DEPOSIT OF FANKOU, GUANGDONG[J]. Acta Sedimentologica Sinica, 1984, 2(3): 34-47.
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