三峡库区黄陵背斜形成机理及与滑坡群关系

doi:10.13278/j.cnki.jjuese.201504117

吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (4): 1142-1154.doi: 10.13278/j.cnki.jjuese.201504117

三峡库区黄陵背斜形成机理及与滑坡群关系

王孔伟¹, 张帆¹, 邱殿明²

1. 三峡大学土木与建筑学院, 湖北宜昌 443002;
2. 吉林大学学报编辑部, 长春 130026

收稿日期:2014-12-24 发布日期:2015-07-26
通讯作者: 邱殿明(1972),男,副编审,主要从事构造地质学方面研究工作,E-mail:qiudm@jlu.edu.cn. E-mail:qiudm@jlu.edu.cn
作者简介:王孔伟(1966),男,副教授,主要从事构造地质方面研究工作,E-mail:wangkongwei@126.com
基金资助:
国家"973"计划前期研究专项课题(2012CB426502);中国地质调查局基础地质调查项目(1212010814057)

Relation of Huangling Anticline and Landslide Group in the Three Gorges Reservoir Area

Wang Kongwei¹, Zhang Fan¹, Qiu Dianming²

1. College of Civil Engineering and Architecture, Three Gorges University, Yichang 443002, Hubei, China;
2. Editorial Department of Journal, Jilin University, Changchun 130026, China

Received:2014-12-24 Published:2015-07-26

摘要/Abstract

摘要：

黄陵背斜、秭归向斜是三峡地区构造地质研究热点之一,前人将其划归于秦岭造山带的组成部分,认为是东西向构造后期改造的结果;分布于此区的仙女山断裂是否穿越长江也是争论的焦点问题之一.这些问题的解决对澄清研究区地质灾害分布特征具有重要意义.笔者在前人研究的基础上,从沉积学、构造地质学角度,在大量野外地质研究工作的基础上,提出了新的看法:黄陵背斜、秭归向斜、当阳向斜、仙女山断裂同属统一的构造体系,其形成和演化与中国东西部构造格局的变迁一致,黄陵背斜具有断层相关褶皱的特点,秭归向斜具有前陆挠曲型盆地构造属性;仙女山断裂形成之初具有传递断层的属性,后期又经历了引张、挤压演化过程,不存在跨越长江向北延伸的问题;受秭归向斜沉降幅度以及东西向构造与南北向构造复合影响,在研究区形成3个滑坡聚集区,分别为贾家店滑坡聚集区、八字门向家店滑坡聚集区、兴山县城附近滑坡聚集区.

关键词: 三峡库区, 黄陵背斜, 秭归向斜, 滑坡群, 秦岭造山带, 仙女山断裂

Abstract:

The study to Huangling anticline-Zigui syncline in the Three Gorges area is hot in the field of structure geology. Predecessors thought that it was the result of a later reformation of the east-west structure, and classified it into Qinling orogenic belt. Another focus is whether Xiannü Mountain fault is across Yangtze River or not. To Solve these problems is of great importance for disclose the distribution of the geological disasters in the study area. The authors put forward a new opinion from sedimentology and tectonics based on the predecessors' studies and a lot of field work by the authors. Huangling anticline, Zigui syncline, Dangyang syncline, and Xiannü Mountain fault belong to one unified tectonic system. This is consistent with the formation and evolution of the fracture of the East-West China. Huangling anticline is the characteristics of fracture related fold, Zigui syncline has a foreland flexural basin syncline tectonic attribute, and Xiannü Mountain fault is the characteristics of the transfer fault with undergoing tension at first and compression later,and not going across Yangze River. Impacted by the east-west and south-north structures as well as Zigui syncline's subsidence range, the landslide accumulation areas are formed such as Jiajiadian landslide accumulation area, Bazimen-Xiangjadian landslide accumulation area, and Xingshan landslide accumulation area.

Key words: the Three Gorges reservoir area, Huangling anticline, Zigui syncline, landslide group, Qinling orogenic belt, Xiannü, Mountain fault

中图分类号:

P542.2

王孔伟, 张帆, 邱殿明. 三峡库区黄陵背斜形成机理及与滑坡群关系[J]. 吉林大学学报(地球科学版), 2015, 45(4): 1142-1154.

Wang Kongwei, Zhang Fan, Qiu Dianming. Relation of Huangling Anticline and Landslide Group in the Three Gorges Reservoir Area[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(4): 1142-1154.

参考文献

[1] 张或丹.黄陵背斜的形成和构造发展初析[J].江汉石油学院学报,1986(1):29-40. Zhang Huodan. Tectonic Evolution and Formation About Huangling Anticline[J].Journal of Jianghan Petroleum Institute,1986(1):29-40.

[2] 陈明是,张树淮.长江三峡地区弧形对突构造特征及形成机制[J].华南地质与矿产,1998 (1):47-55. Chen Mingshi,Zhang Shuhuai. Characteristics and Forming Mechanism of Opposite Protruding Arcuate Structural Zone in the Three Gorges Area of the Yangtze River South China[J].Geology and Mineral Resources of South China,1998 (1):47-55.

[3] 周明礼,秦兴利,冯选朝. 对鄂西仙女山断裂带的几点认识[J].地壳形变与地震,1984,4(1) :82-89. Zhou Mingli,Qin Xingli,Feng Xuanchao.Several Views on Xiannüshan Fault Zone[J].Crustal Deformation and Earthquake,1984,4(1): 82-89.

[4] 谭成轩.长江三峡工程库首区仙女山断裂北延问题研究[J].水文地质与工程地质,1991,18(5):13-17. Tan Chengxuan.North Ward Extension of Xiannüshan Fault in the Front Region of Yangtze Gorges Project[J].Hydrogology and Engineering Geology,1991,18(5):13-17.

[5] 王清云, 李安然,张秋文. 长江三峡地区地球物理异常带地表地质特征[J].地壳形变与地震,1998,18(1): 64-69. Wang Qingyun,Li Anran, Zhang Qiuwen. Surface Geological Charac Teristics of the Yangtze Geophysical Abnormal Beltin the Three Gorge Area[J].Crustal Deformation and Earthquake,1998, 18(1):64-69.

[6] 张广良,张培震,闵伟,等.逆冲-褶皱造山过程中生长地层的识别及应用[J]. 地震地质,2006,28(2):299-307. Zhang Guangliang,Zhang Peizhen, Min Wei,et al. The DentificationI and Application of Growthstra Talinked to the Foreland Fold-and-Thrust Belt During Mounta in Building[J]. Seismology and Geology,2006,28(2):299-307.

[7] 贾东,李一泉,王毛毛,等.断层相关褶皱的三维构造几何学分析:以川西三维地震工区为例[J]. 岩石学报,2011, 27(3):732-740. Jia Dong,Li Yiquan,Wang Maomao,et al.Three-Dimensional Structural Geometryof Fault-Relatedfolds: Examples from 3-Dseismic Explored Blocks in the Western Sichuan Province[J].Acta Petrologica Sinica,2011, 27(3) :732-740.

[8] 李本亮,贾承造,庞雄奇,等.环青藏高原盆山体系内前陆冲断构造变形的空间变化规律[J]. 地质学报,2010, 84(9): 1200-1207. Li Benliang, Jia Chengzao, Pang Xiongqi,et al.The Spatial Distribution of the Foreland Thrust Tectonic Deformation in the Circum Tibetan Plateau Basin and Range System[J]. Acta Geologica Sinica,2010, 84(9):1200-1207.

[9] 渠洪杰,胡健民,崔建军,等.大巴山构造带东段秭归盆地侏罗纪沉积充填过程及其构造演化[J]. 地质学报,2009, 83(9): 1255-1268. Qu Hongjie, Hu Jianmin, Cui Jianjun,et al. Jurassic Sedimentary Filling Process of Zigui Basin in the Eastern Section of Daba Mountain Tectonic Belt and Its Structural Evolution[J]. Acta Geologica Sinica,2010, 84(9): 1200-1207.

[10] 余建华.湖北省秭归盆地层序地层特征[J]. 资源环境与工程,2005, 19(4):257-267. Yu Jianhua. Sequence Stratigraphic Characteristics of Zigui Basin in Hubei[J].Resources Environment and Engineering,2005, 19(4):257-267.

[11] 何登发,吕修祥,林永汉,等.前陆盆地分析[M].北京:石油工业出版社,2009:17-34. He Dengfa,Lü Xiuxiang, Lin Yonghan,et al. Foreland Basin Analysis[M].Beijing:Petroleum Industry Press,2009:17-34.

[12] 朱光,王勇生,王道轩,等.前陆沉积与变形对郯庐断裂带同造山运动的制约[J].地质科学,2006,41(1):102-121. Zhu Guang,Wang Yongsheng,Wang Daoxuan,et al. Constraints of Foreland Sedimentation and Deformation on Synorogenicmotion of the Tan-Lu Fault Zone[J]. Chinese Journal of Geology,2006,41(1):102-121.

[13] 王孔伟,赵小明,邓成进,等. 三峡库区作辑托背斜和巴东断裂与滑坡类型的关系[J].吉林大学学报:地球科学板,2013, 43(1):169-177. Wang Kongwei,Zhao Xiaoming,Deng Chengjin,et al. The Relationship Between Zuojituo Anticline Badong Fault and Landslide in the Three Gorges Reservoir Area[J].Journal of Jilin University:Earth Science Edition,2013,43(1):169-177.

Metrics

Viewed

Full text

562

HTML			PDF

Just accepted	Online first	Issue	Just accepted	Online first	Issue
0	0	0	0	0	562

From	Others	local

Times	213	349
Rate	38%	62%

Abstract

1047

Just accepted	Online first	Issue

0	0	1047

From	Others	local

Times	883	164
Rate	84%	16%

Cited

Web of Science	Crossref	ScienceDirect	Search for Citations in Google Scholar >>


This page requires you have already subscribed to WoS.

Shared

Discussed

三峡库区黄陵背斜形成机理及与滑坡群关系

Relation of Huangling Anticline and Landslide Group in the Three Gorges Reservoir Area

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 10

Metrics

本文评价

推荐阅读 0

[1]	王孔伟, 常德龙, 李春波, 胡安龙, 魏东. 再论“滑坡群”——以三峡库区为例[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1491-1501.
[2]	陈虹，胡健民，武国利，田蜜. 南秦岭构造带中段晚中生代陆内变形特征与侧向挤出构造[J]. 吉林大学学报(地球科学版), 2014, 44(6): 1906-1927.
[3]	陶威，梁文天，张国伟. 南秦岭晚三叠世胭脂坝岩体的磁组构特征及意义[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1575-1586.
[4]	彭令，牛瑞卿，赵艳南，邓清禄. 区域滑坡灾害风险评估--以长江三峡库区秭归县为例[J]. 吉林大学学报(地球科学版), 2013, 43(3): 891-901.
[5]	王孔伟，赵小明，邓成进，张帆. 三峡库区作辑托背斜和巴东断裂与滑坡类型的关系[J]. 吉林大学学报(地球科学版), 2013, 43(1): 169-177.
[6]	陈留勤, 霍荣, 段凯波, 胡水清. 川北前陆盆地上三叠统须家河组陆相层序地层[J]. J4, 2012, 42(3): 600-611.
[7]	牛瑞卿, 彭令, 叶润青, 武雪玲. 基于粗糙集的支持向量机滑坡易发性评价[J]. J4, 2012, 42(2): 430-439.
[8]	叶润青, 牛瑞卿, 邓清禄, 张良培, 赵艳南, 吴婷, 江齐英. 基于多源数据三维可视化集成的高切坡解译[J]. J4, 2012, 42(1): 161-168.
[9]	张加桂. 三峡库区巫山县城秀峰寺-大块子古滑坡特征及形成过程[J]. J4, 2008, 38(3): 448-0454.
[10]	李伟忠,吴冲龙,谭照华. 面向勘察与管理的三峡库区地灾勘察点源信息系统[J]. J4, 2006, 36(03): 424-428.