| 注册
首页|期刊导航|矿产综合利用|桂北地区摩天岭韧性剪切带的应变特征及其构造意义

桂北地区摩天岭韧性剪切带的应变特征及其构造意义

任志丽 秦亚 冯佐海 吴杰 刘诗云 胡乔帆 白玉明 周鹏程

矿产综合利用2025,Vol.46Issue(1):46-60,15.
矿产综合利用2025,Vol.46Issue(1):46-60,15.DOI:10.3969/j.issn.1000-6532.2025.01.005

桂北地区摩天岭韧性剪切带的应变特征及其构造意义

Strain Characteristics of Motianling Ductile Shear Zone in Northern Guangxi and its Tectonic Significances

任志丽 1秦亚 1冯佐海 1吴杰 1刘诗云 2胡乔帆 3白玉明 1周鹏程1

作者信息

  • 1. 桂林理工大学,广西有色隐伏金属矿产勘查与资源高校利用省部共建协同创新中心,广西隐伏金属矿产勘查重点实验室,广西 桂林 541006
  • 2. 广州南方测绘科技股份有限公司,广东 广州 510665
  • 3. 中国有色桂林矿产地质研究院有限公司,广西 桂林 541006
  • 折叠

摘要

Abstract

This is an article in the field of structural geology.In this article,the strain characteristics and tectonic significance of the tile shear zone of Motianling are discussed through macro-microstructure,finite strain measurement of rocks and EBSD structural analysis of quartz.The results show that the Motianling ductile shear zone has typical macro-micro ductile deformation fabrics,including mylonite foliation,rotating porphyry system,S-C fabric,domino structures,asymmetric ocular sphere,quartz dynamic recrystallization,core-mantle structure,mica fish,feldspar mechanical twinning and asymmetric pressure shadow.The finite strain measurement and macro-micro structure shows that the Motianling ductile shear zone extends over 65 km in NNE direction,and its width is 8~12 km.The C-foliation tendency of the mylonite is 220°~356°,the dip angle is 10°~74°,and the extremely dense point occurrence is 285°∠22°.The Motianling ductile shear zone has kinematic characteristics of early sinistral thrust shear and late dextral normal slip shear.The rock strain of Motianling ductile shear zone is mainly flattening strain and tensile strain.At the same time,it shows the shear property of pure shear and simple shear.Quartz EBSD fabric analysis show that the Motianling ductile shear zone is characterized by the late middle-low temperature deformation(300~450℃)superimposed on the early middle-high temperature deformation(400~600℃).The paleo differential stress and strain rate of Motianling ductile shear zone are relatively low,ranging from 10.59~36.31 MPa and 0.63×10-13~87.18×10-13 s-1,respectively.In combination with the above studies and regional geological data,it is considered that the Motianling ductile shear zone was formed in the tectonic setting of recoil after extrusion of the Cathaysia block from SE to the Yangtze block.In the early extrusion and collision stage,the Motianling ductile shear zone has the property of mid-high temperature sinistral thrust shear.After the late orogenic extension,the Motianling ductile shear zone has the property of dextral normal slip shear at mid-low temperature.The above understanding reveals the occurrence,strain characteristics,rheology and dynamics setting of the Motianling ductile shear zone and provides new data for deepening the understand of Caledonian tectonic movement in South China.

关键词

有限应变测量/应变特征/石英EBSD组构/韧性剪切带/桂北摩天岭地区/宏-微观构造/韧性变形/运动学涡度/古差异应力

Key words

Finite strain measurement/Strain charactersitics/Quartz EBSD fabric/Ductile shear zone/Motianling area of northern Guangxi/Macro-micro structure/Ductile deformation/Kinematic vorticity/Paleodifferential stresses

分类

地质学

引用本文复制引用

任志丽,秦亚,冯佐海,吴杰,刘诗云,胡乔帆,白玉明,周鹏程..桂北地区摩天岭韧性剪切带的应变特征及其构造意义[J].矿产综合利用,2025,46(1):46-60,15.

基金项目

广西自然科学基金项目(2022GXNSFAA035570) (2022GXNSFAA035570)

国家自然科学基金项目(42072259) (42072259)

矿产综合利用

1000-6532

访问量1
|
下载量0
段落导航相关论文