| 注册
首页|期刊导航|中国地质|南泥湖一三道庄钼(钨)矿的成岩成矿年龄新数据及其地质意义

南泥湖一三道庄钼(钨)矿的成岩成矿年龄新数据及其地质意义

向君峰 毛景文 裴荣富 叶会寿 王春毅 田志恒 王浩琳

中国地质2012,Vol.39Issue(2):458-473,16.
中国地质2012,Vol.39Issue(2):458-473,16.

南泥湖一三道庄钼(钨)矿的成岩成矿年龄新数据及其地质意义

New geochronological data of granites and ores from the NannihuSandaozhuang Mo(W) deposit

向君峰 1毛景文 2裴荣富 1叶会寿 1王春毅 1田志恒 3王浩琳4

作者信息

  • 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. 南京大学内生金属矿床成矿机制研究国家重点实验室,江苏南京210093
  • 3. 洛阳栾川钼业集团矿山公司.河南洛阳,471542
  • 4. 栾川龙宇钼业有限公司,河南洛阳471500
  • 折叠

摘要

Abstract

The Nannihu-Sandaozhuang molybdenum deposit is the largest porphyry-skam type deposit in eastern Qinling region. This paper reports new LA-ICP-MS zircon U-Pb age data of granitoids (including granitic veins) and ICP-MS molybdenite Re-Os isotopic age data of the samples from the mining area. The obtained formation ages of granitoids are 145.2±1.5 ~ 146.7±1.2Ma, and the model ages of 5 molybdenite samples from stockwork in the Nannihu mining area and 5 molybdenite samples from disseminated skarn in the Sandaozhuang mining area are 143.4±2.0 ~ 146.5±2.3Ma with isochron age of 146.0±l.lMa. These new geochronological data show explicitly that the granitoids and ores were formed simultaneously, suggesting their genetic relationship. Furthermore, these new data have confirmed the existence of magma-thermal event at about 158Ma revealed by previous dating work, and also for the first time revealed that the eastern Qinling area once underwent another magma-thermal event at about 175Ma. The published weighted average age data are of distinct deviation from the real intrusive age of the Nannihu magmatic body, which results from 1) nonhomogeneous origin of zircons in magmatic rock and 2) unrepresentative dating of zircon group.

关键词

东秦岭/华北地台南缘/南泥湖/三道庄/锆石U-Pb年龄/Re-Os年龄

Key words

eastern Qinling/southern margin of the North China Craton/Nannihu/Sandaozhuang/ zircon U-Pb age/Re-Os age

分类

天文与地球科学

引用本文复制引用

向君峰,毛景文,裴荣富,叶会寿,王春毅,田志恒,王浩琳..南泥湖一三道庄钼(钨)矿的成岩成矿年龄新数据及其地质意义[J].中国地质,2012,39(2):458-473,16.

基金项目

中央级公益性科研院所基本科研业务费专项资金(K1018)、南京大学内生金属矿床成矿机制研究国家重点实验室基金项目(15-09-01)、全国危机矿山接替资源找矿项目(20089949和200841019)、国土资源部公益性行业科研专项课题(200911007-08)和国家科技支撑计划项目课题(2010BAB04B06)联合资助 (K1018)

中国地质

OA北大核心CSCDCSTPCD

1000-3657

访问量0
|
下载量0
段落导航相关论文