| 郭忠,肖成东,王自力.冀北大草坪钼矿地质特征及成因探讨[J].地质找矿论丛,2011,26(1):28-33 |
| 冀北大草坪钼矿地质特征及成因探讨 |
| Geological characteristics and genesis of Dacaoping molybdenum deposit in the northern Hebei Province |
| 投稿时间：2010-12-02 |
| DOI：10.6053/j.issn.1001-1412.2011.1. 006 |
| 中文关键词: 大草坪钼矿 地质特征 矿床成因 河北省 |
| 英文关键词:Dacaoping molybdenum deposit geological characteristics deposit genesis Hebei province |
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| 中文摘要: |
| 大草坪钼矿位于冀北上黄旗构造岩浆岩带钼多金属成矿带中,赋矿围岩为花岗岩及花岗闪长岩,成矿时代为燕山期,成矿作用受燕山造山带的控制。研究表明,其成矿物质来源具多源性、多成因、多期次叠加的特征。包裹体液相成分分析显示成矿热液以大气降水为主,包裹体均一化温度为100~360℃,主要在180~220℃范围内;Si,S同位素数据显示成矿流体来源于深部,并与侵入岩体同源,说明大草坪钼矿床属与燕山期岩浆作用有关的中低温热液矿床。 |
| 英文摘要: |
| Dacaoping molybdenum deposit is located in Mo-poly-metal metallogenic belt at Shanghuangqi tectonic-magmatic belt in northern Hebei Province,hosted by granite and granodiorite and formed in Yanshanian period.The metallogeny is controlled by Yanshan orogenic belt.It is characterized by multi-sources,multi-genesis and multi-ore-forming-stage.Ore fluid is mainly meteoric water.Homogenization temperature data of fluid inclusions in range of 100 to 360℃ and concentration between 180 to 220 ℃ indicate that Dacaoping Mo deposit is a meso-epithermal deposit. |
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