邱德同.河台金矿断层岩的地质地球化学特征及其与金矿化的关系[J].地质找矿论丛,1989,(4):12-21 |
河台金矿断层岩的地质地球化学特征及其与金矿化的关系 |
GEOLOGICAL AND GEOCHEMICAL FEATURES OF THE FAULT ROCRS AND THEIR RELATIONSHIP WITH GOLD MINERALIZATITON IN HETAI GOLD DEPOSIT |
|
DOI:10.6053/j.issn.1001-1412.1989.4. 002 |
中文关键词: 断层岩 碎裂岩 糜棱岩 动态重结晶构造 |
英文关键词: |
基金项目: |
|
摘要点击次数: 1270 |
全文下载次数: 1661 |
中文摘要: |
摘要本文论述了河台金矿区断层岩的类型及其地质和地球化学特征,探讨了糜棱岩带与金矿化的关系,指出剪切应变强度和石英动态重结晶发育程度与金矿化强度密切相关. |
英文摘要: |
The author deals with the types of fault rocks and their geological and geochemical feature in Hetai gold district; the relationship between mylonite belt and gold mineralization. The author also indicates the shear strain strength and dynamical recrystallization degree of quartz are closely to related gold mineralization intensity |
查看全文 查看/发表评论 下载PDF阅读器 |
关闭 |