首页 | 本学科首页   官方微博 | 高级检索  
     检索      

豫西铁炉坪银铅矿床矿脉构造解析及近矿蚀变岩绢云母40Ar-39Ar年龄测定
引用本文:高建京,毛景文,陈懋弘,叶会寿,张继军,李永峰.豫西铁炉坪银铅矿床矿脉构造解析及近矿蚀变岩绢云母40Ar-39Ar年龄测定[J].地质学报,2011,85(7):1172-1187.
作者姓名:高建京  毛景文  陈懋弘  叶会寿  张继军  李永峰
作者单位:1. 中国地质大学地质过程与矿产资源国家重点实验室,地球科学与资源学院,北京,100083
2. 中国地质科学院矿产资源研究所国土资源部成矿作用与资源评价重点实验室北京,100037
3. 陕西省地质调查院,西安,710065
4. 河南省有色金属矿产探测工程技术研究中心,郑州,450016
基金项目:国家自然科学基金项目(面上项目,重点项目,重大项目)
摘    要:河南省洛宁县铁炉坪大型脉状银铅矿床地处华北陆块南缘熊耳山中生代变质核杂岩构造西部,由一组主要的NNE走向陡倾斜矿脉和一组次要的NW走向陡倾斜矿脉有规律地组成.矿脉以条带状、角砾状和晶洞-晶簇-梳状三种主要形式多阶段充填而成,按照主要矿脉的矿物共生序列可以分为四个阶段:铁镁碳酸盐阶段(I)、烟灰色石英-贱金属硫化物-银矿...

关 键 词:矿脉  运动学  40  Ar-39  Ar  绢云母  银铅矿  铁炉坪  熊耳山
收稿时间:2011/3/24 0:00:00
修稿时间:4/8/2011 12:00:00 AM

Vein Structure Analysis and 40Ar/39Ar Dating of Sericite from Sub-ore Altered Rocks in the Tieluping Large-size Ag-Pb Deposit of Western Henan Province
GAO Jianjing,MAO Jingwen,CHEN Maohong,YE Huishou,ZHANG Jijun,LI Yongfeng.Vein Structure Analysis and 40Ar/39Ar Dating of Sericite from Sub-ore Altered Rocks in the Tieluping Large-size Ag-Pb Deposit of Western Henan Province[J].Acta Geologica Sinica,2011,85(7):1172-1187.
Authors:GAO Jianjing  MAO Jingwen  CHEN Maohong  YE Huishou  ZHANG Jijun  LI Yongfeng
Institution:China University of Geoscience(Beijing)
Abstract:Abstract The large Tieluping vein-type Ag-Pb ore deposit is located in western Xiongershan metamorphic core complex, south margin of North China Craton. The main Tieluping veins present a paragenesis that can be divided into four stages: an early Fe-Mg carbonates stage (I) prior to polymetallic mineralization, a smoky gray quartz-base metal sulphide - silver minerals stage (II1), a dolomite-white quartz - coarse grained galena - silver minerals stage (II2), and a calcedony-fluorite-calcite stage (III) after the polymetallic mineralization. The ore veins reactivated and reopened the pre-existing ductile shear zones in association with brecciation and open-space filling processes. Kinematic observations demonstrate that the structure of NE ore veins underwent a sinistral and normal motion, and that the structure of NW ore veins underwent dextral and normal motion, correspondingly. 40Ar/ 39Ar dating was performed on sericite from the altered rocks close to the ore veins, which yielded a plateau ages of (134.6 ±1.2) Ma and an isochronal age of (135.3 ±2.4) Ma. This age data corresponds to the sericite 40Ar-39Ar plateau age of (134.9±0.8) Ma for Haopinggou lead-silver veins and the zircon SHRIMP U-Pb age of (133.5±1.4) Ma for Haopinggou granite porphyry in the same ore field, thus further indicates the spatial and temporal consistency of the mineralization and intrusion.
Keywords:Ag-Pb  Tieluping  Xiongershan  vein  kinematic  40Ar-39Ar  sericite
本文献已被 万方数据 等数据库收录!
点击此处可从《地质学报》浏览原始摘要信息
点击此处可从《地质学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号