| 新疆东戈壁斑岩型钼矿床成矿流体包裹体温度——压力研究 |
| |
| 引用本文： | 杨志强,吴邦友,郑松森,陈培伟,安金亮. 新疆东戈壁斑岩型钼矿床成矿流体包裹体温度——压力研究[J]. 地质找矿论丛, 2012, 27(3): 308-314 |
| |
| 作者姓名： | 杨志强 吴邦友 郑松森 陈培伟 安金亮 |
| |
| 作者单位： | 河南省地矿局第二地质勘查院,河南许昌,461000 |
| |
| 摘 要： | 东戈壁斑岩型钼矿床是在新疆境内发现的第一个特大型钼矿,钼资源量(331)+(332)+(333)约503 474.66 t,矿石平均品位0.115％.矿床的形成与隐伏斑状花岗岩体有关,矿化的主要载体是以石英脉、钾长石脉为主的各种脉体,即该矿床兼具斑岩型及脉型矿床的特征.通过对含矿脉体中流体包裹体的研究,初步确定矿床的成矿温度为197～390℃,成矿压力为531.04×105～752.10×105 Pa,成矿深度为1.68～2.39 km,成矿流体为富含多种气态组分的低盐度流体；成矿时代为华力西晚期；矿床成因类型应为浅成中高温岩浆热液型钼矿床.
|
| 关 键 词： | 东戈壁钼矿 斑岩型 流体包裹体 成矿温度—压力—深度 新疆维吾尔自治区 |
| 收稿时间： | 2011-05-04 |
Analysis of metallogenic conditions of East Gobi porphyry molybdenum deposit |
| |
| YANG Zhi-qiang,WU Bang-you,ZHENG Song-sen,CHEN Pei-wei and AN Jin-liang. Analysis of metallogenic conditions of East Gobi porphyry molybdenum deposit[J]. Contributions to Geology and Mineral Resources Research, 2012, 27(3): 308-314 |
| |
| Authors: | YANG Zhi-qiang WU Bang-you ZHENG Song-sen CHEN Pei-wei AN Jin-liang |
| |
| Affiliation: | (The 2nd Institute of Geology and Mineral Exploration,Henan Bureau of Geologyand mineral resources,xuchang 461000,Henan,China) |
| |
| Abstract: | The East Gobi porphyry molybdenum deposit is a newly discovered super-large ore deposit in Xinjiang.Mo metal resources/reserves(331) +(332) +(333) is estimated at 503 474.66 tons with an average grade of 0.115% Mo.Formation of the Mo deposit is related to a concealed porphyritic granite body.Mineralization occurs mainly in veins dominated by quartz vein and K-feldspar vein so the deposit shares characteristics of quartz vein type deposit and porphyry deposit.Study on fluid inclusions shows that the deposit is a meso-high temperature magmatic hydrothermal fluid Mo deposit formed at shallower depth and at temperature 197 to 390 ℃ and pressure 531.04×105 to 752.10×105 Pa in Hercynian Period. |
| |
| Keywords: | East Gobi Mo deposit porphyry Mo deposit ore-forming temperature,pressure and depth Xinjiang |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《地质找矿论丛》浏览原始摘要信息 |
|
点击此处可从《地质找矿论丛》下载免费的PDF全文 |
