试论凡口大型层控铅锌矿床的地质特征及矿床成因

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试论凡口大型层控铅锌矿床的地质特征及矿床成因

陈耀钦, 曾波夫

文章导航 > 沉积学报 > 1984 > 2(3): 34-47

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 1984, 2(3): 34-47.

引用本文:

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 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.

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 1984, 2(3): 34-47.

引用本文:

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 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.

试论凡口大型层控铅锌矿床的地质特征及矿床成因

地质矿产部宜昌地质矿产研究所

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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

摘要: 凡口大型层控铅锌矿床位于广东省北部,中上泥盆纪湘、桂、粤海盆的东部边缘。产于加里东运动后中上泥盆系近底部的碳酸盐岩中。有关它的成因曾提出过礁控成矿、成岩改造及火山成矿等见解。笔者两年来做了较多研究工作,本文将对地质特征和矿床成因于以讨论。

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.

参考文献(1)

[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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文章访问数: 473
HTML全文浏览量: 18
PDF下载量: 487
被引次数: 0

试论凡口大型层控铅锌矿床的地质特征及矿床成因

地质矿产部宜昌地质矿产研究所

收稿日期: 1982-12-16
刊出日期: 1984-09-10

摘要: 凡口大型层控铅锌矿床位于广东省北部,中上泥盆纪湘、桂、粤海盆的东部边缘。产于加里东运动后中上泥盆系近底部的碳酸盐岩中。有关它的成因曾提出过礁控成矿、成岩改造及火山成矿等见解。笔者两年来做了较多研究工作,本文将对地质特征和矿床成因于以讨论。

English Abstract

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 1984, 2(3): 34-47.

引用本文:

陈耀钦, 曾波夫. 试论凡口大型层控铅锌矿床的地质特征及矿床成因[J]. 沉积学报, 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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