| 蒋振和,谢本德,孙立军,玄力,付庆,施国红,张殿华.辽西肖家营子钼矿地质特征及成矿控制因素[J].矿产勘查,2012,3(4):446-451 |
| 辽西肖家营子钼矿地质特征及成矿控制因素 |
| Geological characteristics and metallogenetic factors of Xiaojiayingzi Mo deposit in western Liaoning |
| 投稿时间：2011-12-26 |
| DOI： |
| 中文关键词: 钼矿 地质特征 成矿控制因素 辽西肖家营子 |
| 英文关键词: Mo deposit geological characteristics metallogenetic factors Xiaojiayingzi in western Liaoning |
| 基金项目:原中国有色金属工业总公司华北地台北缘多金属成矿带(辽西段)地质找矿项目(编号:1989-23)资助。 |
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| 中文摘要: |
| 肖家营子钼矿床位于华北地台北缘燕山铜钼成矿带东段,受区域断裂构造、燕山期斑状细粒闪长岩和蓟县系雾迷山组白云质灰岩所控制,并在不同空间先后形成了斑岩型钼矿、夕卡岩型铜钼铁矿和裂隙充填型银铅锌矿。通过对矿床地质特征的分析,总结了该区成矿控制因素,认为区域找矿前景广阔。 |
| 英文摘要: |
| Xiaojiayingzi Mo deposit is located in the north edge of North China Platform, the east of Yanshan Cu-Mo ore-forming belt. By the control of regional faults,Yanshanian porphyritic fine-grained diorite and Jixian-System Wumishan-group dolomitic limestone, with the rock intrusion, it is formed the Mo-Porphyry, Skarns type Cu-Mo-Fe ore and Fissure filling type Ag-Pb-Zn deposits in different space,and a unified metallogenic series is formed. Through the analysis on geological characteristics and further summarization of metallogenic factors, it is considered that there are good prospecting prospect. |
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