|
|||||
|
|
| 内蒙古柳坝沟金矿床石英和黄铁矿的稀土元素地球化学特征及成矿意义 | |
| 引用本文： | 张岩,顾雪祥,章永梅,程文斌,孙雨沁.内蒙古柳坝沟金矿床石英和黄铁矿的稀土元素地球化学特征及成矿意义[J].矿物岩石地球化学通报,2012,31(1):23-30. |
| 作者姓名： | 张岩 顾雪祥 章永梅 程文斌 孙雨沁 |
| 作者单位： | 1. 山东省地质科学实验研究院,山东济南250013;山东省金属矿产成矿地质过程与资源利用重点实验室,山东济南250013 2. 中国地质大学地质过程与矿产资源国家重点实验室,北京,100083 3. 山东省地质科学实验研究院,山东济南250013;山东省金属矿产成矿地质过程与资源利用重点实验室,山东济南250013;中国地质大学地质过程与矿产资源国家重点实验室,北京100083 |
| 基金项目： | 国家自然科学基金资助项目，国家重点基础研究发展计划项目，长江学者和创新团队计划资助，高等学校创新引智计划，中国人民武装警察部队科研项目 |
| 摘 要： | 内蒙古柳坝沟金矿床位于华北地台北缘,是一个典型的以广泛发育钾长石化为重要特色的金矿床.柳坝沟矿床中矿体的石英和黄铁矿的稀土元素特征显示其早期(钾长石化阶段)成矿流体为高温、相对还原的,晚期成矿流体温度逐渐降低.石英和黄铁矿Eu正异常大小是本区寻找石英-钾长石脉型金矿的重要标型特征,Eu正异常越明显,含矿性越好.柳坝沟矿区313#脉矿体中部(163勘探线附近)以及163勘探线以东区域为下一步找矿重点区域,深部寻找石英-钾长石脉型金矿的可能性较大. |
| 关 键 词： | 稀土元素 成矿流体 成矿预测 柳坝沟金矿床 内蒙古 |
Geochemical Characteristics of Rare Earth Elements and Its Significance in the Mineralization of Quartz and Pyrite in the Liubeigou Gold Deposit, Inner Mongolia |
|
| ZHANG Yan , GU Xue-xiang , ZHANG Yong-mei , CHENG Wen-bin , SUN Yu-qin.Geochemical Characteristics of Rare Earth Elements and Its Significance in the Mineralization of Quartz and Pyrite in the Liubeigou Gold Deposit, Inner Mongolia[J].Bulletin of Mineralogy Petrology and Geochemistry,2012,31(1):23-30. | |
| Authors: | ZHANG Yan GU Xue-xiang ZHANG Yong-mei CHENG Wen-bin SUN Yu-qin |
| Institution: | 1,2,3 1.Shandong Institute and Laboratory of Geological Sciences,Shandong,Jinan 250013,China;2.Shandong Key Laboratory of Geological processes and resource utilization in metallic minerals,Shandong Jinan,250013,China;3.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China |
| Abstract: | Liubagou gold deposit,lying in the north margin of North China Craton,is a typical deposit characterized by largely potash feldspathization.Geological characteristics of rare earth elements in quartz and pyrite of the Liubagou gold deposit show that the early ore-forming fluid(K-feldspar) is hypothermal and reductive,and that the ore-forming fluid temperature decreases gradually.The Eu positive anomaly of quartz and pyrite is an important typomorphic characteristic for exploring the quartz and K-feldspar vein type gold deposits,and the Eu positive anomaly is proportional to ore-bearing potential.The middle and east parts of No.313 vein in the Liubagou gold deposit are the key prospecting areas.It is very possible to find the quartz and K-feldspar vein type gold deposit in the deep region. |
| Keywords: | rare earth element ore-forming fluid metallogenic prediction liubagou gold deposit Inner Mongolia |
| 本文献已被 CNKI 万方数据 等数据库收录！ | |