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玉树地区东莫扎抓和莫海拉亨铅锌矿床Rb-Sr和Sm-Nd等时线年龄及其地质意义
引用本文:田世洪,杨竹森,侯增谦,刘英超,高延光,王召林,宋玉财,薛万文,鲁海峰,王富春,苏嫒娜,李真真,王银喜,张玉宝,朱 田,俞长捷,于玉帅.玉树地区东莫扎抓和莫海拉亨铅锌矿床Rb-Sr和Sm-Nd等时线年龄及其地质意义[J].矿床地质,2009,28(6):747-758.
作者姓名:田世洪  杨竹森  侯增谦  刘英超  高延光  王召林  宋玉财  薛万文  鲁海峰  王富春  苏嫒娜  李真真  王银喜  张玉宝  朱 田  俞长捷  于玉帅
作者单位:1. 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
2. 中国地质科学院地质研究所,北京,100037
3. 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;中国地质科学院地质研究所,北京,100037
4. 中国地质调查局,北京,100037
5. 中国地质科学院地质研究所,北京,100037;有色金属矿产地质调查中心,北京,100012
6. 青海省地质调查院,青海,西宁,810012
7. 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;东华理工大学,江西,抚州,344000
8. 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;昆明理工大学,云南,昆明,650093
9. 南京大学现代分析中心,江苏,南京,210093
基金项目:"十一五"国家科技支撑计划重大项目,国家973项目,国土资源大调查项目,中央级公益性科研院所基本科研业务费专项资金,中国博士后科学基金,国家基础研究计划973项目,南京大学内生金 
摘    要:青海玉树地区的东莫扎抓和莫海拉亨铅锌矿床是"三江"北段铜铅锌多金属成矿带铅锌矿床的典型代表,处于玉树逆冲推覆构造带的前锋带位置.本文利用单矿物闪锌矿和共生矿物组合黄铁矿与方铅矿Rb-Sr等时线方法以及共生矿物组合闪锌矿与黄铁矿Sm-Nd等时线方法测定东莫扎抓矿床的成矿时代为34.7~35.7 Ma,平均为35 Ma;利用单矿物闪锌矿和共生矿物组合闪锌矿与方铅矿Rb-Sr等时线方法以及单矿物萤石和共生矿物组合方解石与萤石Sin-Nd等时线方法测定莫海拉亨矿床的成矿时代为31.8~33.9 Ma,平均为33 Ma,表明2个矿床的成矿时代基本一致,为同期同源成矿作用的产物.结合区域成矿地质背景,建立了2个矿床的构造控矿模式.此外,本文获得的玉树地区典型铅锌矿床的成矿时代与"三江"南段兰坪盆地和"三江"北段沱沱河盆地铅锌矿床的成矿时代相近,证明青藏高原东部和北部受逆冲推覆控制的长达1 000 km的狭长地带有望成为一条巨型Pb-Zn成矿带.

关 键 词:地球化学  Rb-Sr等时线  Sm-Nd等时线  共生矿物组合  成矿时代  逆冲推覆构造  构造模式  青海玉树东莫扎抓和莫海拉亨铅锌矿床

Rb-Sr and Sm-Nd isochron ages of Dongmozhazhua and Mohailaheng Pb-Zn ore deposits in Yushu area, southern Qinghai and their geological implications
TIAN ShiHong,YANG ZhuSen,HOU ZengQian,LIU YingChao,GAO YanGuang,WANG ZhaoLin,SONG YuCai,XUE WanWen,LU HaiFeng,WANG FuChun,SU AiNa,LI ZhenZhen,WANG YinXi,ZHANG YuBao,ZHU Tian,YU ChangJie,YU YuShuai.Rb-Sr and Sm-Nd isochron ages of Dongmozhazhua and Mohailaheng Pb-Zn ore deposits in Yushu area, southern Qinghai and their geological implications[J].Mineral Deposits,2009,28(6):747-758.
Authors:TIAN ShiHong  YANG ZhuSen  HOU ZengQian  LIU YingChao  GAO YanGuang  WANG ZhaoLin  SONG YuCai  XUE WanWen  LU HaiFeng  WANG FuChun  SU AiNa  LI ZhenZhen  WANG YinXi  ZHANG YuBao  ZHU Tian  YU ChangJie  YU YuShuai
Abstract:Dongmozhazhua and Mohailaheng Pb-Zn deposits in Yushu area of Qinghai Province are representative Pb-Zn deposits in the Cu-Pb-Zn polymetallic mineralization belt of the northern part of the Nujiang-Lancangjiang-Jinshajiang area, which are in the front belt of Yushu thrust nappe system. The ages of the Dongmozhazhua de posit have been determined by the Rb-Sr isochron method for sphalerite and one group of intergrowth mineral as semblage samples (pyrite and galena) and the Sm-Nd isochron method for one group of intergrowth mineral as semblage samples (sphalerite and pyrite); whereas, the ages of the Mohailaheng deposit have been determined by the Rb-Sr isochron method for sphalerite and one group of intergrowth mineral assemblage samples (spha lerite and galena) and the Sm-Nd isochron method for fluorite and one group of intergrowth mineral assemblage samples (calcite and fluorite). The ages of Dongmozhazhua and Mohailaheng deposits are 34.7-35.7 Ma with an average of 35 Ma and 31.8~33.9 Ma with an average of 33 Ma, respectively, implying they have the same mineralization epoch. Combined with geological and geochemical data, it is concluded that the Dongmozhazhua and Mohailaheng deposits formed during the same geological event and the metals have the same source. Togeth er with regional mineralization geological setting, a possible tectonic model for metallogeny of Dongmozhazhua and Mohailaheng Pb-Zn deposits has been established. These two ages are close to the ages of the Pb-Zn deposit in Lanping basin of the southern part of the Nujiang-Lancangjiang-Jinshajiang area and in Tuotuohe basin of the northern part of the Nujiang-Lancangjiang-Jinshajiang area, indicating that it is possible that the narrow 1000 km - length belt controlled by thrust nappe system in the eastern and northern margins of Tibetan plateau would be a giant Pb-Zn mineralization belt.
Keywords:geochemistry  Rb-Sr isochron  Sm-Nd isochron  mineral assemblage  ore-forming epoch  thrust nappe system  tectonic model  Dongmozhazhua and Mohailaheng Pb-Zn deposits in Yushu area  Qinghai Province
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