|本期目录/Table of Contents|

[1]陈秀其.江南古陆东北缘盖层叠加褶皱特征[J].地球科学与环境学报,2019,41(01):15-28.
　CHEN Xiu-qi.Characteristics of the Capping Superposed Fold in the Northeastern Margin of Jiangnan Orogen, China[J].Journal of Earth Sciences and Environment,2019,41(01):15-28.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第01期
页码:
15-28
栏目:
基础地质与矿产地质
出版日期:
2019-01-15

文章信息/Info

Title:
Characteristics of the Capping Superposed Fold in the Northeastern Margin of Jiangnan Orogen, China
文章编号:
1672-6561(2019)01-0015-14
作者:
陈秀其
1.合肥工业大学 资源与环境工程学院，安徽 合肥 230009； 2.安徽省地质调查院，安徽 合肥 230001
Author(s):
CHEN Xiu-qi
1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China； 2. Geological Survey of Anhui Province, Hefei 230001, Anhui, China
关键词:
构造地质; 叠加褶皱; 赤平投影; 区域尺度; 干涉样式; 应力场; 构造序列; 江南古陆
Keywords:
tectonic geology;  superposed fold;  stereographic projection;  regional scale;  interference pattern;  stress field;  tectonic sequence;  Jiangnan orogen
分类号:
P542+.2
DOI:
-
文献标志码:
A
摘要:
江南古陆东北缘古生代—早中生代盖层中发育的褶皱构造属性逐渐被认识，但该区是否存在叠加褶皱及其叠加样式如何则未见报道。通过野外调查，发现江南古陆东北缘发育加里东期、印支期褶皱构造。通过对区内叠加褶皱特征和应力场恢复研究，并应用构造解析和赤平投影法研究叠加褶皱的几何学和运动学特征，显示盖层发育3期区域性叠加褶皱变形：区内早期遭受SN向挤压，形成加里东晚期近EW向褶皱(第一期褶皱)；其后遭受SE—NW向挤压，形成印支早期NE向或NNE向褶皱(第二期褶皱)；晚期遭受NE—SW向挤压，形成印支晚期—燕山早期近SN向或NNW向褶皱(第三期褶皱)。区域叠加褶皱主要有横跨和斜跨叠加褶皱，发育多样干涉样式。结果表明：第二期褶皱斜跨第一期褶皱，形成了区内基本构造格局。深入研究叠加褶皱构造特征和变形演化史，对区内构造格架重建和地质找矿均具有重要意义。
Abstract:
The tectonic attribute of the capping fold developed in Paleozoic-Early Mesozoic in the northeastern margin of Jiangnan orogen is gradually recognized, but there is not research report about the superposed folds and their superposed patterns in the study area at present. Based on the field investigates, Caledonian and Indosinian fold structures develop in the northeastern margin of Jiangnan orogen. Based on the characteristics of the superposed folds and the restoration of stress field, the geometry and kinematics characteristics of superposed folds are discussed by structure analysis and stereographic projection method, and there are three stages of the capping superposed fold deformation, including the first fold (F1), the second fold (F2) and the third fold (F3). In the early stage, the cap suffers SN compression, and forms Late Caledonian EW-nearly fold (F1); then, the first fold suffers SE-NW compression, and forms Early Indosinian NE or NNE fold (F2); in the later stage, the second fold suffers NE-SW compression, and forms Late Indosinian-Early Yanshanian SN-nearly or NNW fold (F3). The regional superposed folds mainly have vertical span and slant span styles, and develop various Interference patterns. The results show that the second fold diagonally overprints the first fold, and forms the basic structural pattern in the area. The study on the structural characteristics and deformation evolution of superposed folds has great significance on the reconstruction of tectonic framework and geological prospecting.

参考文献/References:

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相似文献/References:

[1]刘浪,李致伟,邵俊琦,等.滇东北会泽地区叠加褶皱特征及构造演化[J].地球科学与环境学报,2018,40(05):595.
　LIU Lang,LI Zhi-wei,SHAO Jun-qi,et al.Superimposed Fold Characteristics and Tectonic Evolution in Huize Area of Northeastern Yunnan, China[J].Journal of Earth Sciences and Environment,2018,40(01):595.

备注/Memo

备注/Memo:
收稿日期:2018-06-11;修回日期:2018-10-02
基金项目:国家自然科学基金国际(地区)合作与交流项目(41320104003);中国地质调查局地质调查项目(1212011120851,1212011120848)
作者简介:陈秀其(1968-),男,安徽全椒人,安徽省地质调查院高级工程师,合肥工业大学理学博士研究生,E-mail:chenxiuqiac@sina.com。
更新日期/Last Update: 2019-01-25