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首页|期刊导航|地质学报(英文版)|40Ar/39Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai,East China

40Ar/39Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai,East China

LI Jinyi YANG Tiannan CHEN Wen ZHANG Sihong

地质学报(英文版)2003,Vol.77Issue(2):155-168,14.
地质学报(英文版)2003,Vol.77Issue(2):155-168,14.

40Ar/39Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai,East China

40Ar/39Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai,East China

LI Jinyi 1YANG Tiannan 1CHEN Wen 1ZHANG Sihong1

作者信息

  • 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037
  • 折叠

摘要

Abstract

Recent investigations reveal that the ultrahigh-pressure metamorphic (UHPM) rocks in the Donghai regionof East China underwent ductile and transitional ductile-brittle structural events during their exhumation. The earlierductile deformation took place under the condition of amphibolite facies and the later transitional ductile-brittledeformation under the condition of greenschist facies. The hanging walls moved southeastward during both of these twoevents. The 40Ar/39Ar dating of muscovites from muscovite-plagioclase schists in the Haizhou phosphorous mine, whichare structurally overlain by UHPM rocks, yields a plateau age of 218.0±2.9 Ma and isochron age of 219.8Ma, indicatingthat the earlier event of the ampibolite-facies deformation probably took place about 220 Ma ago. The 40Ar/39Ar dating oforiented amphiboles parallel to the movement direction of the hanging wall on a decollement plane yields a plateau age of213.1 ±0.3 Ma and isochron age of 213.4±4.1 Ma, probably representing the age of the later event. The dating of pegmatiticbiotites and K-feldspars near the decollement plane from the eastern Fangshan area yield plateau ages of 203.4±0.3 Ma,203.6±0.4 Ma and 204.8±2.2 Ma, and isochron ages of 204.0±2.0 Ma, 200.6±3.1 Ma and 204.0±5.0 Ma, respectively,implying that the rocks in the studied area had not been cooled down to closing temperature of the dated biotites and K-feldspars until the beginning of the Jurassic (about 204 Ma). The integration of these data with previous chronological ageson the ultrahigh-pressure metamorphism lead to a new inference on the exhumation of the UHPM rocks. The UHPM rocksin the area were exhumed at the rate of 3-4 km/Ma from the mantle (about 80-100 km below the earth's surface at about240 Ma) to the lower crust (at the depth of about 20-30km at 220 Ma), and at the rate of 1-2 km/Ma to the middle crust (atthe depth of about 15 km at 213 Ma), and then at the rate of less than 1 km/Ma to the upper crust about 10 km deep at about204 Ma.

关键词

ultrahigh-pressure metamorphic rocks, structural deformation, 40Ar/39Ar dating, exhumation, Donghai, East China

Key words

ultrahigh-pressure metamorphic rocks, structural deformation, 40Ar/39Ar dating, exhumation, Donghai, East China

分类

天文与地球科学

引用本文复制引用

LI Jinyi,YANG Tiannan,CHEN Wen,ZHANG Sihong..40Ar/39Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai,East China[J].地质学报(英文版),2003,77(2):155-168,14.

基金项目

This study was financially supported by the former Ministry of Geology and Mineral Resources of China (grant No. 9501102). (grant No. 9501102)

地质学报(英文版)

1000-9515

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