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含刚玉变沉积岩对扬子克拉通西北缘新元古代演化史的制约

张易 王浩铮 冯林峰 刘恒 薛帅朕 郭杰 崔夏红

地质科学2024,Vol.59Issue(4):940-960,21.
地质科学2024,Vol.59Issue(4):940-960,21.DOI:10.12017/dzkx.2024.067

含刚玉变沉积岩对扬子克拉通西北缘新元古代演化史的制约

Constraints of corundum bearing metasedimentary rocks on the Neoproterozoic evolution history of the northwest margin of the Yangtze Craton

张易 1王浩铮 2冯林峰 1刘恒 1薛帅朕 1郭杰 1崔夏红3

作者信息

  • 1. 西南石油大学油气藏地质及开发工程全国重点实验室,地球科学与技术学院 成都 610500
  • 2. 西南石油大学油气藏地质及开发工程全国重点实验室,地球科学与技术学院 成都 610500||西南石油大学火成岩综合地质研究所,天然气地质四川省重点实验室 成都 610500
  • 3. 河北地质大学 石家庄 050031
  • 折叠

摘要

Abstract

Clarifying the Precambrian metamorphic basement exposed on the northwest margin of the Yangtze Craton is of fundamental significance for revealing the tectonic evolution history of the Yangtze Craton in the Neoproterozoic and the formation and occurrence mechanism of deep resources in the Sichuan Basin.This article reveals petrogenesis of biotite plagioclase gneiss and corundum bearing sillimanite cordierite schist in the Micangshan terrane on the northwest edge of the Yangtze Craton.Combined with metamorphic research,it is believed that the formation of corundum bearing mica schist is related to the loss of SiO2 in the deep melting process of the coexisting biotite plagioclase gneiss.The temperature and pressure during the metamorphic peak recorded by the migmatitic biotite plagioclase gneiss reached 759 ℃~770 ℃,0.48~0.55 GPa(with a geothermal gradient of 46 ℃/km~53 ℃/km),while the typical mineral assemblage of corundum bearing sillimanite cordierite schist records the P-T conditions of 580 ℃~620 ℃,0.36~0.46 GPa(with a geothermal gradient of 35 ℃/km~43 ℃/km).Metamorphic zircons have reported two sets of metamorphic ages,814±9 Ma and 736±17 Ma.Based on previous research results,this article believes that the sedimentary rocks containing corundum have further finely characterized the arc-continent collision process since~814 Ma.The high temperature gradient may be related to the involvement of mantle derived materials during the collision process,and the corresponding collision process further confirms that the Yangtze Craton is located on the periphery of the Rodinia supercontinent.

关键词

含刚玉变沉积岩/扬子克拉通/新元古代/变质作用

Key words

Corundum bearing metasedimentary rocks/Yangtze Craton/Neoproterozoic/Metamorphism

分类

天文与地球科学

引用本文复制引用

张易,王浩铮,冯林峰,刘恒,薛帅朕,郭杰,崔夏红..含刚玉变沉积岩对扬子克拉通西北缘新元古代演化史的制约[J].地质科学,2024,59(4):940-960,21.

基金项目

国家自然科学基金项目(编号:42072225,41702199)资助 (编号:42072225,41702199)

地质科学

OA北大核心CSTPCD

0563-5020

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