| 徐庆华,陆海,董德仁.辽宁省岫岩县石庙子金矿床地质特征及控矿因素[J].地质找矿论丛,2013,28(2):244-248 |
| 辽宁省岫岩县石庙子金矿床地质特征及控矿因素 |
| Geological characteristics and ore-controlling factors of Shimiaozi Gold deposit in Xiuyuan county, Liaoning Province |
| 投稿时间：2013-01-22 |
| DOI：10.6053/j.issn.1001-1412.2013.02.012 |
| 中文关键词: 石庙子金矿 地质特征 岩浆热液 “S”形展布构造 找矿标志 辽宁省 |
| 英文关键词:Shimiaozi Gold deposit geological characteristics magmatic hydrothermal fluid “S”fracture prospecting mark Liaoning Province |
| 基金项目: |
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| 摘要点击次数: 1895 |
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| 中文摘要: |
| 岫岩石庙子金矿床产于似斑状黑云二长花岗岩体中,受"S"形展布的追踪断裂构造带控制;具有典型岩浆热液金矿床成因特点。在NE向"S"形展布的断裂构造中,构造复合部位对成矿有利;构造的转弯处储矿条件较好,金的品位相对较高。 |
| 英文摘要: |
| Shimiaozi Gold deposit in Xiuyuan county, Liaoning Province occurs in porphyric biotite monzonitic granite body and is controlled by a traceable "S"fracture. It is characteristic of magmatic hydrothermal gold deposit. The "S"fracture is in NE direction consisting of several fractures. Overprinting localities of the fractures are the conductive fracture of ore fluid and bends of the "S"fracture favorable for the ore fluid accumulation where higher grade ore generally occur. |
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