| 内蒙古红花尔基钨钼矿云英岩化白云母Ar-Ar定年及其地质意义 |
| |
| 引用本文： | 向安平,佘宏全,陈毓川,秦大军,王亚军,韩增光,康永建.内蒙古红花尔基钨钼矿云英岩化白云母Ar-Ar定年及其地质意义[J].岩矿测试,2016,35(1):108-116. |
| |
| 作者姓名： | 向安平 佘宏全 陈毓川 秦大军 王亚军 韩增光 康永建 |
| |
| 作者单位： | 中国地质科学院矿产资源研究所, 北京 100037;中国地质大学资源学院, 湖北 武汉 430074,中国地质科学院矿产资源研究所, 北京 100037,中国地质科学院矿产资源研究所, 北京 100037,内蒙古第六地质矿产勘查开发院, 内蒙古 海拉尔 021008,内蒙古第六地质矿产勘查开发院, 内蒙古 海拉尔 021008,内蒙古第六地质矿产勘查开发院, 内蒙古 海拉尔 021008,中国地质科学院矿产资源研究所, 北京 100037 |
| |
| 基金项目： | 中国地质调查局地质调查项目——大兴安岭关键构造-岩浆-成矿事件研究(1212011120992);国家基础科研项目——大兴安岭中北段中生代多金属矿成矿系统研究(2013CB429800) |
| |
| 摘 要： | 红花尔基钨多金属矿是近年在大兴安岭中北部地区发现的一处大型钨多金属矿床,主要矿化蚀变为云英岩化、绢英岩化,主要有用金属矿物为白钨矿和辉钼矿,岩体内辉钼矿与白钨矿有上钼下钨的带状分布特点,地质特征显示该矿床为一高温热液型钨(钼)矿床。为准确限定成矿热液活动时间,本文对矿区典型蚀变矿物——云英岩化蚀变带白云母进行Ar-Ar同位素定年,获得Ar-Ar坪年龄为174.4±1.2 Ma,等时线年龄为173.2±4.3 Ma。根据矿区云英岩化带与钨钼矿化带空间上重合和密切共生的关系,可知白云母的形成是与白钨矿、辉钼矿形成同源、同时,且辉钼矿Re-Os年龄(176.8±2.2 Ma)与Ar-Ar年龄在误差范围内具有一致性,该年龄代表了钨钼矿热液成矿时代。结合野外地质特征及锆石U-Pb、辉钼矿Re-Os年龄,进一步限定该矿床成矿时代为早中侏罗世,属燕山期构造岩浆活动的产物。
|
| 关 键 词： | 红花尔基钨矿 高温热液型钨多金属矿床 白云母 Ar-Ar定年 大兴安岭中北段 燕山期 |
| 收稿时间： | 2015/8/13 0:00:00 |
| 修稿时间： | 1/7/2016 12:00:00 AM |
Ar-Ar Age of Muscovite from the Greisenization Alteration Zones of the Honghuaerji Tungsten Polymetallic Deposit,Inner Mongolia,and Its Geological Significance |
| |
| XIANG An-ping,SHE Hong-quan,CHEN Yu-chuan,QIN Da-jun,WANG Ya-jun,HAN Zeng-guang and KANG Yong-jian.Ar-Ar Age of Muscovite from the Greisenization Alteration Zones of the Honghuaerji Tungsten Polymetallic Deposit,Inner Mongolia,and Its Geological Significance[J].Rock and Mineral Analysis,2016,35(1):108-116. |
| |
| Authors: | XIANG An-ping SHE Hong-quan CHEN Yu-chuan QIN Da-jun WANG Ya-jun HAN Zeng-guang and KANG Yong-jian |
| |
| Institution: | Institute of Mineral Resources, China Academy of Geology Sciences, Beijing 100037, China;China University of Geology Sciences, Wuhan 430074, China,Institute of Mineral Resources, China Academy of Geology Sciences, Beijing 100037, China,Institute of Mineral Resources, China Academy of Geology Sciences, Beijing 100037, China,The Sixth Institute of Geological Mineral Exploration in Inner Mongolia, Hailaer 021008, China,The Sixth Institute of Geological Mineral Exploration in Inner Mongolia, Hailaer 021008, China,The Sixth Institute of Geological Mineral Exploration in Inner Mongolia, Hailaer 021008, China and Institute of Mineral Resources, China Academy of Geology Sciences, Beijing 100037, China |
| |
| Abstract: | The newly found Honghuaerji tungsten polymetallic deposit is a large scale tungsten deposit in north-east Daxinganling in China.The alteration includes sericitization and greisenization.The metallic minerals are scheelite and molybdenite.These minerals in rock body show the belt characteristics of W in the top and Mo in the bottom.Geological characteristics indicate that it is a high temperature hydrothermal deposit.In order to constrain the timing of hydrothermal activities,Ar-Ar dating of muscovite from the greisenization alteration zones was carried out.The Ar-Ar dating yields an Ar-Ar plateau age of 174.4±1.2 Ma and an isochron age of 173.2±4.3 Ma.Because greisenization alteration zones and the tungsten(molybdenum) mineralization belt are closely related in space,muscovite,scheelite,and molybdenite may have formed simultaneously.Moreover,the Ar-Ar age of muscovite is in agreement with the Re-Os age of molybdenite(176.8±2.2 Ma) within uncertainties,indicating this Ar-Ar age represents the timing of the tungsten and molybdenum hydrothermal mineralization.Combined field geology,U-Pb ages and Re-Os ages indicate this deposit formed the Jurassic period and may be the product of Yanshanian tectonic magmatic activity. |
| |
| Keywords: | Honghuaerji tungsten deposit high temperature hydrothermal type polymetallic deposit muscovite Ar-Ar daling the mid and north parts of Greater Khingan Range the Yanshanian |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《岩矿测试》浏览原始摘要信息 |
| 点击此处可从《岩矿测试》下载免费的PDF全文 |
|
