[1]郭建华,朱美衡,刘辰生.2005.湖南桑植—石门复向斜走廊剖面构造特征分析.大地构造与成矿学,29(2):215-222.
 GUO Jianhua,ZHU Meiheng,LIU Chensheng.2005.STRUCTURAL CHARACTERISTICS OF THE CORRIDOR SECTION IN SANGZHI-SHIMEN SYNCLINORE.Geotectonica et Metallogenia,29(2):215-222.
点击复制

湖南桑植—石门复向斜走廊剖面构造特征分析
分享到:

《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2005年29卷02期
页码:
215-222
栏目:
构造地质学
出版日期:
2005-05-25

文章信息/Info

Title:
STRUCTURAL CHARACTERISTICS OF THE CORRIDOR SECTION IN SANGZHI-SHIMEN SYNCLINORE
作者:
郭建华1朱美衡1刘辰生1刘学锋2张或丹2王明艳1
1.中南大学 地学与环境工程学院, 湖南 长沙 410083; 2. 长江大学,湖北 荆州 434023
Author(s):
GUO Jianhua1 ZHU Meiheng1 LIU Chensheng1 LIU Xuefeng2 ZHANG Huodan2 and WANG Mingyan1
1. Central South University, Changsha, Hunan 410083, China; 2. Yangtze University, Jingzhou, Hubei 434023, China
关键词:
桑植—石门复向斜 构造样式 构造滑脱面 变形机制
Keywords:
Sangzhi-Shimen synclinore structural pattern slip surface of structure formation mechanism
分类号:
P542
文献标志码:
A
摘要:
为了查明桑植—石门复向斜的地表、地下构造特征及其相互间的关系,采取了详细的地表走廊剖面的测量,以及结合地震勘探资料和大地电磁测深(MT)资料的综合解释。桑植—石门复向斜可进一步划分为四个次一级的构造带,从北向南依此是:堰塘湾构造带、四望山构造带、江垭构造带及教子垭构造带。江垭构造带和教子垭构造带的地面构造特征与地下构造特征具有一致性,基本上为构造简单的北倾斜坡;而四望山构造带的地面构造特征与地下构造特征存在着明显的不协调性。这种变形特征可解释为沿盖层间滑脱面的逆冲,以及断弯背斜的形成,上覆构造层中的褶皱向下消失在滑脱面上,形成所谓的“无根褶皱”。
Abstract:
A ground geological survey and an interpretation on synthesis of seismic data and MT data for the corridor section of the Sangzhi-Shimen synclinore are used to study the properties of both the ground structure and the underground structure of the Sangzhi-Shimen synclinore as well as the relationship between them. The Sangzhi-Shimen synclinore can be divided into four para-tectonic belts. From north to south, they are Yantangwan tectonic belt, Siwangshan tectonic belt, Jiangya tectonic belt and Jiaoziya tectonic belt. Based on the comprehensive analysis of MT profile data and seismic data for the Jiaoziya structure belt and Jiangya structure belt, it is found that the ground tectonic shape is essentially according to that of the underground structure. However, in the Siwangshan structure belt, the ground structure is not according to the underground structure. Through analysis of the slip surface and tectonic pattern, the discordances of the ground structure and the underground one can be accountered for by the thrust of the decollement and the formation of fault-curve anticline. This kind of fold resulted from the covering tectonic layers disappears in the decollement surface, which leads to the formation of the non-rooted folds.

参考文献/References:

段太忠,曾允孚,高振中.1988.根据沉积历史分析华南古大陆边缘构造演化.石油与天然气地质,9(4):410-420.
贾宝华.1994.湖南雪峰隆起区构造变形研究.中国区域地质,36(1):65-71.
马文璞,李学军,刘和甫等.1993.雪峰隆起的构造性质及其对上扬子东南缘古生代盆地的改造.见:江南雪峰地区的层滑作用及多期复合构造.北京:地质出版社.
任纪舜.1989.中国东部及邻区大地构造演化的新见解.中国区域构造,31(4):289-300.
水涛.1987.中国东南大陆基底构造格局.中国科学(B缉),(4):414-422.
王鸿桢,杨森楠,李思田.1983.中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展.地质学报,57(3):213-223.
王燮培,费琪,张家骅.1990.石油勘探构造分析.武汉:中国地质大学出版社.
许靖华,孙枢,李继亮.1987.是华南造山带而不是地台.中国科学(B缉),(11):1107-1115.
许效松,徐强,潘桂棠等.1996.中国南大陆演化与全球古地理对比.北京:地质出版社.
Duan Taizhong, Zeng Yunfu and Gao Zhenzhong. 1988. Analysis of tectonic evolution of paleocontinental margin in South China based of sedimentary history. Oil and Gas Geology, 9(4): 410-420 (in Chinese with English abstract).
Hsu K J, Li Jiliang, Chen Haihong, Wang Qingchen, Sun Shu and Sengor A M C. 1990. Tectonics of South China: Key to understanding West Pacific geology. Tectonophysics, 183: 9-39.
Hsu K J, Sun Shu and Li Jiliang. 1987. Huanan Alps, not South China platform. Sci Sin (Ser B), 1107-1115 (in Chinese).
Hsu K J, Sun Shu, Li Jiliang, Chen Haihong, Pen Haipo and Sengor A M C. 1988. Mesozoic overthrust tectonics in South China. Geology, 16: 418-421.
Jia Baohua.1994.Tectonic deformation of the Xuefeng uplift area in Hunan. Regional Geology of China, 36(1): 65-71 (in Chinese with English abstract).
Ma Wenpu, Li Xuejun, Liu Hepu et al. 1993. The tectonic property of the Xuefeng uplift and its alteration on the Paleozoic basins on the south-east margin of the upper Yangtze platform. In: Layer decollement and multi-time compound structure in the Xuefeng area, south of the Yangtze River. Beijing: Geological Publishing House (in Chinese).
Mitra S. 1986. Duplex structures and imbricate thrust systems: Geometry, structural position, and hydrocarbon potential. AAPG, 70(6): 1087-1112.
Mitra S. 1990. Fault-propagation folds: Geometry, kinematics evolution, and hydrocarbon. AAPG, 74(6): 921-945.
Ren Jishun. 1989. Some new ideas on tectonic evolution of Eastern China and adjacent areas. Regional Geology of China, 31(4): 289-300 (in Chinese with English abstract).
Shui Tao. 1987. The structure framework of the continent basement in southeastern China. Science in China (B), (4): 414-422 (in Chinese).
Suppe J. 1983. Geometry and kinematics of fault-bend folding. American Journal of Science, 283(4): 684-721.
Wang Hongzhen, Yang Sennan and Li Sitian. 1983. Mesozoic and Cenozoic basin formation in east China and adjacent regions and development of the continental margin. Acta Geologica Sinica, 51(3):213-223 (in Chinese with English abstract).
Wang Xiepei, Fei Qi and Zhang Jiahua. 1990. The tectonic analysis on petroleum exploration. Wuhan: China University of Geoscience Press (in Chinese).
Xu Xiaosong, Xu Qiang and Pan Guitang et al. 1996. Evolution of South China continental and contrast of global palaeogeography. Beijing: Geological Publishing House (in Chinese).

相似文献/References:

[1]付宜兴,张萍,李志祥.中扬子区构造特征及勘探方向建议.大地构造与成矿学,2007.31(3):308.
 FU Yixing,ZHANG Ping,LI Zhixiang.THE TECTONIC CHARACTERISTICS AND THEIR SIGNIFICANCE FOR HYDROCARBON EXPLORATION IN MIDYANGTZE AREA.Geotectonica et Metallogenia,2007.29(2):308.
[2]刘新民,郭战峰.鄂东南地区印支期以来构造变形特征及油气意义.大地构造与成矿学,2006.3(1):018.
 LIU Xinmin and GUO Zhanfeng.TECTONIC DEFORMATION SINCE INDOSINIAN PERIOD AND ITS SIGNIFICANCE FOR HYDROCARBON IN SOUTHEAST HUBEI.Geotectonica et Metallogenia,2006.29(2):018.
[3]佘晓宇,丁小辉,梁斌.江汉平原东部构造特征与演化.大地构造与成矿学,2012.36(2):209.
 SHE Xiaoyu,DING Xiaohui,LIANG Bin.Structural Style and Tectonic Evolution of the Eastern Part of Jianghan Basin in the Jianghan Plain Region.Geotectonica et Metallogenia,2012.29(2):209.
[4]谢玉洪,童传新,范彩伟.琼东南盆地断裂系统特征与演化.大地构造与成矿学,2015.39(5):795.doi:10.16539/j.ddgzyckx.2015.05.004
 XIE Yuhong,TONG Chuanxin,FAN Caiwei.Characteristics and Evolution of Fault System in Qiongdongnan Basin.Geotectonica et Metallogenia,2015.29(2):795.doi:10.16539/j.ddgzyckx.2015.05.004
[5]陈秀其,周涛发*,李龙明.皖南—浙西地区盖层褶皱构造形迹特征.大地构造与成矿学,2018.42(2):193.doi:10.16539/j.ddgzyckx.2018.02.001
 CHEN Xiuqi,ZHOU Taofa* and LI Longming.Characteristics of Capping Fold Structure in the Southern Anhui and Western Zhejiang Regions.Geotectonica et Metallogenia,2018.29(2):193.doi:10.16539/j.ddgzyckx.2018.02.001
[6]钱建平,张 果,漆炜博.甘肃早子沟金矿复合成矿构造系统的构成、样式、时间演化和控矿规律.大地构造与成矿学,2018.优先出版:001.doi:10.16539/j.ddgzyckx.2020.02.018
 QIAN Jianping,ZHANG Guo,QI Weibo.The Composition, Style, Time Evolution and Ore-controlling Rules of Compound Metallogenic Structural System of Zaozigou Gold Deposit, Gansu Province.Geotectonica et Metallogenia,2018.29(2):001.doi:10.16539/j.ddgzyckx.2020.02.018
[7]钱建平,张 果,漆炜博.甘肃早子沟金矿复合成矿构造系统的构成、样式、演化和控矿规律.大地构造与成矿学,2020.44(5):913.doi:10.16539/j.ddgzyckx.2020.02.018
 QIAN Jianping,ZHANG Guo,QI Weibo.Composition, Pattern, and Evolution of Compound Metallogenic Structural System and Their Controls on Mineralization of Zaozigou Gold Deposit, Gansu Province.Geotectonica et Metallogenia,2020.29(2):913.doi:10.16539/j.ddgzyckx.2020.02.018
[8]樊 燏,刘 强,任利民.山西太原西山东缘(晋祠-平泉)构造变形特征及其地质意义.大地构造与成矿学,2018.优先出版:001.doi:10.16539/j.ddgzyckx.2020.05.016
 FAN Yu,LIU Qiang and REN Limin.Structural Features of the Eastern Margin of the Xi Mountain in Taiyuan, Shanxi Province and its Geological Significances.Geotectonica et Metallogenia,2018.29(2):001.doi:10.16539/j.ddgzyckx.2020.05.016

备注/Memo

备注/Memo:
收稿日期:2004-08-11;改回日期:2004-10-28作者简介:郭建华(1957-),男,博士(后),教授,博士生导师,主要从事石油勘探开发的教学与科研工作. Email: gjh796@mail.csu.edu.cn① 江汉石油管理局勘探开发研究院. 1996. 湖北神农架红花—湖南桃源牛车河油气勘探地质大剖面综合研究.
更新日期/Last Update: 2005-05-15