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中国东部中生代构造格局与演化
Mesozoic Tectonic Framework and Evolution of Eastern China

查看参考文献35篇

侯泉林 1   林伟 2   许德如 3   闫全人 1   刘庆 1   何苗 1   王智琳 2   卫巍 4   郭谦谦 1  
文摘 中国东部早中生代以挤压构造为主,如大别造山带的逆冲推覆构造,而晚中生代伸展构造十分显著,表现为大量发育的变质核杂岩、同构造岩浆岩、拆离断层带以及穹隆构造等,这些伸展构造使地壳深部的岩石折返至地表,从而使中下地壳结构发生了强烈的改造。拟通过对中国东部晚中生代构造发育的典型地区:北部的燕山构造带、中-东部的大别-苏鲁构造带和东部的东南沿海构造带进行系统的研究、分析、归纳和总结,恢复燕山运动启动前的构造体制,研究中国东部对多幕次燕山运动中地壳变形对板块相互作用及其深部过程的响应,阐明中国东部燕山期构造体制转折的期次、时限、动力学演变机制及其与板块运动的关系,进而探讨其对成矿作用的制约。
其他语种文摘 Eastern China was dominated by compressional structures in early Mesozoic but vast extensional structures in the Late Mesozoic. A large number of extensional structures,such as metamorphic core complexes,syntectonic plutons, detachments and domes,have exhumed the middle to lower crust into surface,and changed the structure of middle-lower crust dramatically. This paper aims to investigate the late Mesozoic structures in typical areas of Eastern China that include Yanshan tectonic belt in the north,Dabie-Sulu tectonic belt in the central and the coastal tectonic belt in the southeast. This project will also try to reconstruct the tectonic framework before Yanshanian period for its critical role to know how crust deformation responded to interaction and deep process of plates during the Yanshanian period. The purpose of this project is to illuminate the tectonic phase,activity time,dynamic mechanism,and relationship to relevant plates in Eastern China during Yanshanian period,and discuss the constraint on the metallic mineralization.
来源 矿物岩石地球化学通报 ,2017,36(6):1063-1067 【核心库】
DOI 10.3969/j.issn.1007-2802.2017.06.023
关键词 晚中生代 ; 伸展构造 ; 变质核杂岩 ; 动力学机制
地址

1. 中国科学院大学, 北京, 100049  

2. 中国科学院地质与地球物理研究所, 北京, 100029  

3. 中国科学院广州地球化学研究所, 广州, 510640  

4. 中南大学, 长沙, 410083

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 地质学
基金 国家重大研发计划项目
文献收藏号 CSCD:6165427

参考文献 共 35 共2页

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引证文献 3 篇

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