| 高建伟.山东金翅岭金矿成矿构造及应力场研究[J].地质与勘探,2014,50(1):122-129 |
| 山东金翅岭金矿成矿构造及应力场研究 |
| Metallogenic structure and Tectonic Stress Field of the Jinchiling Gold Deposit in Shandong Province |
| 投稿时间：2012-05-21 修订日期：2013-01-05 |
| DOI： |
| 中文关键词: 构造变形 构造应力场 石英脉型金矿 金翅岭金矿 山东招远 |
| 英文关键词: tectonic deformation tectonic stress field quartz-vein type gold deposit Zhaoyuan, Shandong province |
| 基金项目:中国地质调查局“全国危机矿山找矿”项目（20089937）资助 |
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| 中文摘要: |
| [摘 要]金翅岭金矿位于胶东西北部招远—莱州的中部，为石英脉型金矿。基于构造填图和古构造应力场反演，初步查明了该矿床控矿断裂的运动学特征和构造演化历史。研究表明：在侏罗系—白垩系时期，该矿床控矿断裂大致经历三期活动：成矿前构造应力场为NW-SE向挤压，成矿期为NE-SW向挤压，成矿后为NW-SE向挤压；成矿作用发生在构造应力场从NW-SE挤压到NE-SW向挤压转换时期。正是由于构造应力场转化使得控矿断裂开启，才导致成矿作用的发生。 |
| 英文摘要: |
| Abstract: The Jinchiling quartz-vein type gold deposit is located in the central part of the Zhaoyuan-Lizhou metallogenic belt. Structural mapping and paleo-tectonic stress inversion reveal the tectonic movement features and tectonic evolution history of the Jinchiling gold deposit. The result shows that during the Jurassic to the Cretaceous period，the ore-control fault of this deposit underwent three stages of activities: (1) nearly NW-SW-directed compression stress before mineralization; (2) during mineralization, the stress field changed into NE-SW compression; and (3) the stress field converted to NW-SE compression again after mineralization. Mineralization occurred in the transformation period of the tectonic stress field. The mineralization occurred when the tectonic stress field transformed as aforementioned，which opened the ore-control fault and led to filling of ore bodies． |
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