北京怀柔崎峰茶-得田沟金矿田断裂构造及其控矿作用

北京怀柔崎峰茶-得田沟金矿田断裂构造及其控矿作用

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文章导航 > 地质力学学报 > 1998 > 4(2): 21-29

李中坚, 陈柏林, 董法先, 王平安, 王世发, 李怀永. 北京怀柔崎峰茶-得田沟金矿田断裂构造及其控矿作用[J]. 地质力学学报, 1998, 4(2): 21-29.

引用本文:

李中坚, 陈柏林, 董法先, 王平安, 王世发, 李怀永. 北京怀柔崎峰茶-得田沟金矿田断裂构造及其控矿作用[J]. 地质力学学报, 1998, 4(2): 21-29.

Li Zhongjian, Chen Bailin, Dong Faxian, Wang Ping'an, Wang Shifa, Li Huaiyong. FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION[J]. Journal of Geomechanics, 1998, 4(2): 21-29.

Citation:

Li Zhongjian, Chen Bailin, Dong Faxian, Wang Ping'an, Wang Shifa, Li Huaiyong. FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION[J]. Journal of Geomechanics, 1998, 4(2): 21-29.

北京怀柔崎峰茶-得田沟金矿田断裂构造及其控矿作用

1.
中国地质科学院地质力学研究所

2.
北京市地质调查所

3.
北京市地矿局101队

收稿日期: 1998-03-28

修回日期: 1998-04-28

刊出日期: 1998-04-28

FAULT SYSTEMS IN THE QIFENGCHAN-DETIANGOU GOLD FIELD OF HUAIROU,BEIJING,AND ITS CONTROL OF GOLD MINERALIZATION

1.
Institute of Geomechanics, CAGS

2.
Beijing Geological Survey

3.
No.1 Prospecting Party, BGMR, Beijing

Received Date: 28 March 1998

Revised Date: 28 April 1998

Publish Date: 28 April 1998

摘要: N-S向断裂带与E-W向断裂带是崎峰茶-得田沟金矿田内主要赋矿构造带,具有韧-脆性变形特征;金的矿化富集与断裂带中糜棱岩及石英脉的发育密切相关;矿体定位于断裂带形变相变相对强烈的部位或区段。
- 金矿田 /
- 断裂构造 /
- 控矿作用
Abstract: In the Qifengcha-Detiangou gold field,the N-S-trending and E-W-trending fault zones are the major ore-bearing structural zones,which are characterized by ductile-brittle deformation.Mineralization of gold is closely related to mylonites and quartz veins.Gold bodies are confined to part of fault zones where occur stronger deformation and facies changes of rock and minerals.
- gold field /
- fault system /
- control of gold mineralization

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