| 潘鸿迪,申萍.陕西镇安丘岭微细浸染型金矿床形成与岩石和构造的关系[J].地质与勘探,1999,(5):16-19 |
| 陕西镇安丘岭微细浸染型金矿床形成与岩石和构造的关系 |
| THE FORMATION OF THE QIULING SEDIMENTS-HOSTED DISSEMINATED GOLD DEPOSIT IN ZHENAN, SHANXI AND ITS RELATIONS WITH ROCKS AND STRUCTURES |
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| DOI： |
| 中文关键词: 微细浸染型金矿 不纯细碎屑岩、碳酸盐岩系列岩石 韧性剪切构造 丘岭 |
| 英文关键词: ductile shear structure, unpure clastic-carbonate rocks, ductile shear structure, sediments-hosted disseminated gold ores, Qiuling |
| 基金项目: |
| 潘鸿迪 申萍 |
| [1]西安工程学院 [2]西安矿业学院 |
| 摘要点击次数: 2014 |
| 全文下载次数: 1219 |
| 中文摘要: |
| 丘岭微细浸染型金矿床产于上古生界南羊山组及袁家沟组地层中。研究表明，金矿形成与不纯细碎屑岩—碳酸盐岩系列岩石和叠加在其上的韧性剪切构造有密切关系，受岩性和构造控制 |
| 英文摘要: |
| The Qiuling sediments-hosted disseminated gold deposit in Zhenan, Shanxi is hosted in Nanyangshan Formation and Yuanjiagou Formation of Upper Paleozoic. Controlled by lithology and structure, its metallogenesis is related to unpure clastic-carbonate rocks and the overlapping ductile shear structures. |
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