大别山-苏鲁碰撞造山带构造几何学、运动学和岩石变形分析

林伟 王清晨 石永红

大别山-苏鲁碰撞造山带构造几何学、运动学和岩石变形分析

林伟王清晨石永红

- 中国科学院地质与地球物理研究所、岩石圈国家重点实验室,北京100029
基金项目:
国家重点基础研究发展规划（G1999075506）,国家自然科学基金NSFC（40472116,40202021）的资助.感谢郭敬辉研究员提供的建设性修改意见.野外工作得到了国家重点基础研究发展规划[G1999075506],国家自然科学基金NSFC（40472116,40202021）的资助.日本学术振兴会提供了林伟在日研究费用[JSPS02060].

收稿日期: 2005-04-30

刊出日期: 2005-07-31

Architecture, kinematics and deformation analysis in Dabie-Sulu collision zone

LIN Wei, WANG QingChen ,SHI YongHong

- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beifing 100029, China

Received Date: 30 April 2005

Publish Date: 31 July 2005

摘要

摘要: 按照构造几何学特点和运动学特征我们把大别山-苏鲁造山带的分为三个构造单元：南部，中部和北部。造山带南部为一套构造堆叠体系；中部为一个混合岩穹窿，浅变质的砂岩、板岩和片岩构成了大别山-苏鲁造山带的北部构造单元。造山带南部的构造堆叠体系主要由前陆褶皱带构成：未变质的新元古代-早三叠世的沉积地层；由“宿松群”北部和苏北地区的“海州群”构成的高压变质岩石单元及含柯石英和金刚石的超高压变质岩石单元。造山带中部的混合岩穹隆由大别山地区的罗田穹隆和苏鲁地区的莱西-栖霞穹隆构成。同样大别山北部的浅变质“佛子岭-卢镇关群”和胶东地区浅变质的“蓬莱群”构成了造山带北部的构造堆叠体系。同时大别山和苏鲁两个构造地体均经历了相似的多期构造变形：沿NW—SE向矿物拉伸线理发育的上部指北的剪切变形代表着造山带主变形期的变形；早期向南逆冲的韧性剪切变形和沿中部混合岩穹隆边缘发育的重力滑脱变形体系，后者代表了混合岩穹隆形成时的垂向缩短作用。正是由于构造几何学和多期变形的可对比性决定了这两个变质地体具有相同的地球动力学背景。
- 大别-苏鲁碰撞造山带 /
- 构造几何学 /
- 运动学 /
- 岩石多期变形
- Dabie-Sulu collision zone /
- Geometry /
- Kinematics /
- Polyphase deformation

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大别山-苏鲁碰撞造山带构造几何学、运动学和岩石变形分析

Architecture, kinematics and deformation analysis in Dabie-Sulu collision zone

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