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湖南大义山、塔山岩体锆石U-Pb年龄及其构造意义

李勇 张岳桥 苏金宝 李建华 董树文

地球学报Issue(3):302-311,10.
地球学报Issue(3):302-311,10.DOI:10.3975/cagsb.2015.03.05

湖南大义山、塔山岩体锆石U-Pb年龄及其构造意义

Zircon U-Pb Dating of Dayishan and Tashan Plutons in Hunan Province and Its Tectonic Implications

李勇 1张岳桥 2苏金宝 3李建华 4董树文3

作者信息

  • 1. 北京大学,北京 100871
  • 2. 中国地质科学院地质力学研究所,北京 100081
  • 3. 中国地质科学院地质力学研究所,北京 100081
  • 4. 河海大学,江苏南京 210098
  • 折叠

摘要

Abstract

The distribution and intrusion of Early Mesozoic granites in central South China such as Dayishan pluton and Tashan pluton are closely related to folded structure in this region. Precise chronologic studies can constrain the age of the tectonic deformation. This paper report zircon U-Pb LA-ICP-MS ages of the southern part of Dayishan pluton based on dating of 3 samples:the age of the eastern margin is (171.8±1.9) Ma, that of the western margin is (169.9±1.8) Ma and that of the central part is (164.2±2.6) Ma. The zircon U-Pb LA-ICP-MS age of the eastern part of Tashan pluton is (247±5.9) Ma. Dayishan pluton experienced two phases of intrusion between 164.2 and 171.8 Ma and formed a composite pluton;after that, it experienced rapid uplift prior to 125 Ma, and then it was rapidly raised to the surface at the cooling rate of 1°C/Ma. Dayishan pluton and Tashan pluton recorded Indosinian and Yanshanian magmatic activities. The EW-trending structural zone controlled Indosinian granites, such as Yangmingshan and Tashan; the ages of Dayishan and Qitianling plutons constrain the Yanshanian tectonic deformation, and the formation of the NNE-trending folds in South China should be earlier than (171.8±1.9) Ma.

关键词

华南地区/大义山岩体/塔山岩体/锆石U-Pb年龄

Key words

South China/Dayishan pluton/Tashan pluton/zircon U-Pb age

分类

天文与地球科学

引用本文复制引用

李勇,张岳桥,苏金宝,李建华,董树文..湖南大义山、塔山岩体锆石U-Pb年龄及其构造意义[J].地球学报,2015,(3):302-311,10.

基金项目

本文由财政部“深部探测技术与实验研究”专项之子课题(编号:Sinoprobe-08-01)资助。 (编号:Sinoprobe-08-01)

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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