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江西景德镇地区中生代推覆构造变形特征与年代学约束

霍海龙 欧阳永棚 张达 陈正乐 毕珉烽 陈国华 贺晓龙 李宁 李兴俭 薛伟

地质力学学报2018,Vol.24Issue(1):9-24,16.
地质力学学报2018,Vol.24Issue(1):9-24,16.DOI:10.12090/j.issn.1006-6616.2018.24.01.002

江西景德镇地区中生代推覆构造变形特征与年代学约束

DEFORMATION CHARACTERISTICS AND GEOCHRONOLOGICAL CONSTRAINTS OF MESOZOIC NAPPE STRUCTURE IN JINGDEZHEN AREA, NORTHEASTERN JIANGXI

霍海龙 1欧阳永棚 2张达 3陈正乐 1毕珉烽 2陈国华 4贺晓龙 3李宁 1李兴俭 1薛伟1

作者信息

  • 1. 中国地质大学(北京)地球科学与资源学院,北京100083
  • 2. 中国地质科学院地质力学研究所,北京100081
  • 3. 江西省地质矿产勘查开发局九一二大队,江西鹰潭335001
  • 4. 中国地质科学院矿产资源研究所,北京100037
  • 折叠

摘要

Abstract

Jingdezhen area is located in the northeastern Jiangxi province,which belongs to the Yangzi plate,and has undergone long-term tectonic activities.According to the study of regional tectonic section,the Mesozoic thrust-nappe structure direction of the study area is from NW to SE,the upper Shuangqiaoshan group has been pushed to the top of Carboniferous-Triassic strata,and the structural styles of the thrust belt are characterized by imbricate fans and duplexes and the maximum principal compressive stress is SE-NW trend.The study of undeformed granite zircon U-Pb isotope dating shows that the U-Pb isotope age is 157 ~ 172 Ma,and the time of tectonic movement is during early Yanshanian period.The Mesozoic thrust-nappe structure produced the magmatic mineralization process in the Jingdezhen area,and the granites of Jingdezhen area may have invaded from intracontinental subductionrelated transformation tectonic setting during the early Yanshanian.The nappe structure constrains the magmatic evolution and in space associated with mineralization.Then it controls the mineralization process of the deposit.

关键词

景德镇地区/中生代/逆冲推覆构造/年代学

Key words

Jingdezhen area/Mesozoic/thrust-nappe structure/chronology

分类

天文与地球科学

引用本文复制引用

霍海龙,欧阳永棚,张达,陈正乐,毕珉烽,陈国华,贺晓龙,李宁,李兴俭,薛伟..江西景德镇地区中生代推覆构造变形特征与年代学约束[J].地质力学学报,2018,24(1):9-24,16.

基金项目

公益性行业科研专项(201411035-3) (201411035-3)

国家科技支撑计划项目(2015BAB05B04-01,2015BAB05B04-02) (2015BAB05B04-01,2015BAB05B04-02)

中国地质调查局项目(DD20160053) (DD20160053)

地质力学学报

OACSCDCSTPCD

1006-6616

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