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桂东南大容山晚二叠世花岗岩锆石U-Pb年龄和Sr-Nd-Hf同位素特征及其地质意义

王磊 龙文国 周岱 徐旺春 金鑫镖

地质通报2016,Vol.35Issue(8):1291-1303,13.
地质通报2016,Vol.35Issue(8):1291-1303,13.

桂东南大容山晚二叠世花岗岩锆石U-Pb年龄和Sr-Nd-Hf同位素特征及其地质意义

Late Triassic zircon U-Pb ages and Sr-Nd-Hf isotopes of Darongshan gran- ites in southeastern Guangxi and their geological implications

王磊 1龙文国 2周岱 1徐旺春 2金鑫镖1

作者信息

  • 1. 武汉地质矿产研究所,湖北武汉430205
  • 2. 中国地质调查局花岗岩成岩成矿地质研究中心,湖北武汉430205
  • 折叠

摘要

Abstract

The petrogenesis and geodynamic processes of the Darongshan granite have been a subject of much controversy. In this paper, the authors report U-Pb ages and Sr-Nd-Hf isotopes for the Darongshan granite in southeastern Guangxi. LA-ICP-MS U-Pb zircon analysis yielded 206Pb/238U weighted mean age of 253.6±2.1Ma, 256.4±1.8Ma and 256.8±2.8Ma for three granite sam⁃ples respectively, indicating that these granites are of Late Permian origin rather than the Early-Middle Triassic origin. They have relatively high εNd(t) values (-9.18~-13.4) and younger Nd model ages (tDMc=1.55~1.84Ga), which are consistent with εHf(t) val⁃ues (-5.5~-6.7) and Hf model ages (TDM2=1.64~1.71Ga), suggesting an lower crustal source mixed with the Paleo-Mesoproterozoic materials. Combined with previous studies, the authors hold that the Darongshan granitic magmatism might have been related to anatexis of the lower crust due to the subduction/collision between Indosinian block and South China plate during the Hercynian to Indosinian period.

关键词

锆石U-Pb/Sr-Nd-Hf同位素/花岗岩/大容山/桂东南地区

Key words

zircon U-Pb/Sr-Nd-Hf isotope/granite/Darongshan/southeastern Guangxi

分类

天文与地球科学

引用本文复制引用

王磊,龙文国,周岱,徐旺春,金鑫镖..桂东南大容山晚二叠世花岗岩锆石U-Pb年龄和Sr-Nd-Hf同位素特征及其地质意义[J].地质通报,2016,35(8):1291-1303,13.

基金项目

中国地质调查局项目(编号1212011085416、12120113063000)和国家自然科学基金项目 ()

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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