| 南岭诸广山北体复式花岗岩锆石SHRIMP U-Pb年龄及多期岩浆活动 |
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| 引用本文： | 郭爱民,陈必河,陈剑锋,周超,司程山,郑正福.南岭诸广山北体复式花岗岩锆石SHRIMP U-Pb年龄及多期岩浆活动[J].中国地质,2017,44(4):781-792. |
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| 作者姓名： | 郭爱民 陈必河 陈剑锋 周超 司程山 郑正福 |
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| 作者单位： | 湖南省地质调查院, 湖南 长沙 410116,湖南省地质调查院, 湖南 长沙 410116,湖南省地质调查院, 湖南 长沙 410116;中南大学地球科学与信息物理学院, 湖南 长沙 410083,湖南省地质调查院, 湖南 长沙 410116,湖南省地质调查院, 湖南 长沙 410116,湖南省地质调查院, 湖南 长沙 410116 |
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| 基金项目： | 中国地质调查局项目“南岭成矿带中西段地质矿产调查”（121201009000150002）、“湖南桂东地区矿产远景调查”（矿调〔2005〕12-8号）、“湘东地区花岗岩与成矿关系研究”（ 1212011220520）及“湖南浣溪地区1∶5万地质矿产综合调查”（12120115029301）联合资助。 |
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| 摘 要： | 诸广山复式花岗岩基位于湘、赣、粤三省交界处,是南岭花岗岩的重要组成部分,由南体和北体组成,出露面积大于5000 km2,形成于加里东期、印支期、燕山期3个时代。通过对诸广山北体3期花岗岩锆石SHRIMP U-Pb定年,结果表明,加里东期花岗闪长岩锆石SHRIMP U-Pb年龄为(414.5±4.5)Ma(n=13,MSWD=0.52)、(417.3±4.8)Ma(n=12,MSWD=0.84),形成于晚志留世末。印支期黑云母二长花岗岩锆石SHRIMP U-Pb年龄(207.5±2.7)Ma(n=10,MSWD=1.6),形成于晚三叠世末。燕山期二云母二长花岗岩锆石SHRIMP U-Pb年龄(148.2±1.7)Ma(n=13,MSWD=0.93),形成于晚侏罗世。该成果为南岭地区构造-岩浆演化及成矿作用研究,提供了重要的花岗岩年代学依据。
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| 关 键 词： | 花岗岩 锆石U-Pb SHRIMP 诸广山 南岭 |
| 收稿时间： | 2016/3/24 0:00:00 |
| 修稿时间： | 2016/7/18 0:00:00 |
Zircon SHRIMP U-Pb geochronology of granitoids from northern Zhuguangshan granitic composite batholith, Hunan Province |
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| GUO Aimin,CHEN Bihe,CHEN Jianfeng,ZHOU Chao,SI Chengshan and ZHENG Zhengfu.Zircon SHRIMP U-Pb geochronology of granitoids from northern Zhuguangshan granitic composite batholith, Hunan Province[J].Chinese Geology,2017,44(4):781-792. |
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| Authors: | GUO Aimin CHEN Bihe CHEN Jianfeng ZHOU Chao SI Chengshan and ZHENG Zhengfu |
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| Institution: | Hunan Institute of Geological Survey, Changsha 410116, Hunan, China,Hunan Institute of Geological Survey, Changsha 410116, Hunan, China,Hunan Institute of Geological Survey, Changsha 410116, Hunan, China;School of Geoscience and InfoPhysics, Central South University, Changsha 410083, Hunan, China,Hunan Institute of Geological Survey, Changsha 410116, Hunan, China,Hunan Institute of Geological Survey, Changsha 410116, Hunan, China and Hunan Institute of Geological Survey, Changsha 410116, Hunan, China |
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| Abstract: | Zhuguangshan granitic composite batholith situated in Hunan-Jiangxi-Guangdong border area is an important part of Nanling large granite province, with the total area of northern and southern body being greater than 5000 km2. The results of zircon SHRIMP U-Pb geochronology of granitoids of northern Zhuguangshan show that the granitic body was formed in three periods with ages varying from the Caledonian through Indosinian to Yanshannian. Caledonian granodiorite was formed in late Silurian period, Indosinian biotite adamellite was formed in late Triassic period and Yanshannian dimicaceous adamellite was formed in late Jurassic period, with SHRIMP zircon U-Pb ages being (414.5±4.5) Ma, (417.3±4.8) Ma, (207.5±2.7) Ma, and (148.2±1.7) Ma respectively. The results obtained by the authors provide important geochronologic basis for the study of geology and mineralization in this area. |
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| Keywords: | granite zircon U-Pb SHRIMP Zhuguangshan Nanling |
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