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北秦岭官坡地区柯石英榴辉岩变质作用的P-T-t轨迹

METAMORPHIC P-T-t PATH FOR THE COESITE ECLOGITES FROM THE GUANPO AREA, NORTHERN QINLING MOUNTAIN

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【作者】 赵东林

【Author】 Zhao Donglin(Dept. of Economic Resources, Xi’an College of Geology, Xi’an 710054)

【机构】 西安地质学院资源系

【摘要】 根据矿物包裹和替代关系以及共生组合规律,北秦岭官坡地区柯石英榴辉岩的变质作用演化可划分为5个阶段,即前榴辉岩相的绿帘角闪岩相、榴辉岩相、后榴辉岩相的角闪岩相、绿帘角闪岩相和绿片岩相。Sm-Nd同位素定年显示,北秦岭柯石英榴辉岩于400±16Ma沿朱夏断裂被推覆上升,P-T-t轨迹的地球动力学成因可能与扬子和华北陆块间的俯冲-碰撞作用有关。

【Abstract】 On the studies of the relations of mineral generations and conversion of mineral assemblages, the metamorphic evolution of the coesite eclogite in Guanpo area, northern Qinling mountain, may be divided into five stages: epidote-amphibolitic factes of the pre-eclogite factes, coesite eclogite factes, amphibolitic factes of the post-eclogite factes, epidote-amphibolitic factes and greenschist factes. The. Sin-Nd dating of the rock specimen yields an excellent isochron, indicating that the coesite eclogite was uplifted along Zhuxia fault at about 400 Ma ago. The geodynamic process for the P-T-t path of coesite eclogite might be related to the uderthrust collision between Yangtze and Huabei massifs.

【基金】 国家自然科学基金
  • 【文献出处】 西安工程学院学报 ,Journal of Xi’an Engineering University , 编辑部邮箱 ,1997年02期
  • 【分类号】P588.3
  • 【被引频次】5
  • 【下载频次】78
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