长江三峡库区滑坡发育与河道演变的地质过程分析

陈国金; 李长安; 陈松; 邵磊

doi:10.3799/dqkx.2013.040

长江三峡库区滑坡发育与河道演变的地质过程分析

doi: 10.3799/dqkx.2013.040

陈国金^1,,
李长安^2, ,,
陈松³,
邵磊²

1.
湖北省地质环境总站，湖北荆州 434020
2.
中国地质大学教育部长江三峡库区地质灾害研究中心，湖北武汉 430074
3.
武汉市建筑设计院，湖北武汉 430014

基金项目:

国家自然科学基金 40971008

湖北省重点科技攻关计划基金项目 2005AA308B02

湖北省重点科技攻关计划基金项目 NOETZ2008A02

详细信息

作者简介:
陈国金(1942-)，男，正高职高级工程师，主要从事水工环地质与地质灾害防治研究.E-mail: chengj0215@sina.com

通讯作者:
李长安，E-mail: chanli@cug.edu.cn

中图分类号: P534.4
计量
- 文章访问数: 3109
- HTML全文浏览量: 157
- PDF下载量: 584
- 被引次数: 0
出版历程
- 收稿日期: 2012-04-15
- 刊出日期: 2013-03-01

Landslide Development and the Geological Process of Watercourse Evolution in the Three Gorges Reservoir Area

1.
Hubei Geological Environment Station, Jingzhou434020, China
2.
Three Gorges Research Center for Geo-Hazard of Ministry of Education, China University of Geosciences, Wuhan430074, China
3.
Wuhan Architectural Design Institute, Wuhan430014, China

摘要

摘要: 据区域地质灾害调查，三峡库区发育有数以千计的滑坡.年代学研究表明，三峡地区的滑坡均发生于第四纪中更新世中后期，并具有明显的阶段性特征，滑坡的高发期大致为：(41~37)×10⁴ aBP、(31~27)×10⁴ aBP和(17~5)×10⁴ aBP.滑坡发育与区域新构造抬升和河流地貌形成的地质过程相一致，且主要发生在第四纪的间冰期，表明滑坡与构造抬升、气候变暖、长江河道快速下切贯通发展具有一定的耦合关系.三峡地区尚未发现年龄超过54×10⁴ aBP的滑坡，据此推测长江贯通三峡的时间可能在早更新世.
- 三峡 /
- 滑坡 /
- 河道演变 /
- 地质过程 /
- 工程地质
Abstract: According to the regional survey for geo-hazards, thousands of landslides occurred in the Three Gorges reservoir area. Chronology studies show that these landslides mostly occurred after the Mid-Pleistocene and could be divided in 3 stages, namely, (41-37)×10⁴ aBP, (31-27)×10⁴ aBP and (17-5)×10⁴ aBP. These landslides mostly occurred in the interglacial period and could be well related with the regional uplift and geological process of the formation of river landform in the Three Gorges area. Based on these, we conclude that the occurrence of the landslides can be well correlated with tectonic uplift, climate change, rapidly down-cutting and breakthrough development in the Yangtze River. It is inferred that the cut-through timing of the Three Gorges probably be Early Pleistocene mainly owing to the loss of landslides which ages older than 54×10⁴ aBP.
- Three Gorges /
- landslides /
- evolution of the river channel /
- geological process /
- engineering geology

HTML全文

图 1 更新世滑坡年代分布(邓清禄，2000)

Fig. 1. The age of landslide in Pleistocene

下载: 全尺寸图片幻灯片

图 2 长江三峡及邻区新构造运动、地貌过程、气候变化与滑坡事件的相关性分析

Fig. 2. The correlation analysis between landslide and neotectonics, geomorphological process, climate change in Three Gorges and adjacent areas

下载: 全尺寸图片幻灯片

表 1 三峡库区古滑坡绝对年龄(邓清禄，2000)

Table 1. The age of paleo-landslide in Three Gorges area

序号	滑坡名	样品	测定方法	年龄(10⁴ aBP)	资料来源
1	杨家岭	平洞滑带土	TL	2.7	长江水利委员会勘测总队报告，1990
2	大坪	滑带土	TL	27.7±1.39	湖北省水文队报告, 1989, 1995
3	谭家湾	平洞滑带土	TL	7.48±2.24	长江水利委员会勘测总队报告，1990
4	新滩	平洞滑带土	TL	4.46±0.89	长江水利委员会勘测总队报告，1990
5	黄腊石大石板	平洞滑带土	TL	10.58 ±2.68 12±3.6	湖北省水文队报告, 1989, 1995
6	黄腊石石榴树包	滑带土	TL	29.55±2.36	湖北省水文队报告, 1989, 1995
7	台子角	滑带土	ESR	8.58 ±2.57 8.06±2.58	湖北省水文队报告, 1989, 1995
8	赵树岭	滑带土	TL	11.68±0.9	长江水利委员会综合勘测局报告，1996
9	黄土坡滑坡(上部)	滑带土石英	TL	39.25 41.2 37.29	湖北省水文队报告, 1991, 2001
10	曲尺盘	滑带土	ESR	9.1±1.8	长江水利委员会综合勘测局报告，1996
11	百换坪	滑带土	TL	33.14±1.65	长江水利委员会综合勘测局报告，1996
12	藉塘		TL	16~17	长江水利委员会综合勘测局报告，1996
13	故陵		ESR ESR TL	12.6 ±0.63 12.46±1.03 14.28 ±1.20	长江水利委员会综合勘测局报告，1996
14	旧县坪西滑体	滑带土	TL ESR	2.92 ±0.14 5.61±1.68	长江水利委员会综合勘测局，1996
15	茨草沱	滑带土	TL	26.6±1.33	长江水利委员会综合勘测局报告，1996

下载: 导出CSV

参考文献(22)

[1]	Cai, Y.J., Wang, J.H., Zhu, Y.F., et al., 2010. Study on Revolution History and Formation Environment of the Shigu-Hutiaoxia Section of Jinsha River. Resources Environment & Engineering, 24(3): 283-286 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HBDK201003017.htm
[2]	Chen, G.J., Chen, S., Jian, J.Z., 2005. Groundwater Influence on the Reservoir-Type and Rainfall-Type Landslides. In: A Collection of Academic Theses on Prevention and Control of Geohazards in the Three Gorges Reservoir Region of Hubei Province. China University of Geosciences Press, Wuhan (in Chinese).
[3]	Chen, S., Chen, G.J., Xu, G.L., 2008. Mechanism of Geological Processes of Formation and Deformation of the Huangtupo Landslide. Earth Science—Journal of China University of Geosciences, 3(3): 411-415 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DQKX200803018.htm
[4]	Deng, Q.L., 2000. Slope Deformation Structures-Analysis of Badong New County Slope. China University of Geosciences Press, Wuhan (in Chinese).
[5]	Li, C.A., 1997a. The Coupling of Physiographic, Tectonic-Climate and Geological Hazard. Earth Science Frontiers, 4(3-4): 204 (in Chinese with English abstract).
[6]	Li, C.A., 1997b. Relationship of Landslip with Tectonic Movement and Climatic Change in Yangtze Three Gorges. Geological Science and Technology Information, 16(3): 88-91 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ703.018.htm
[7]	Liu, C.Z., 2005. On the Evolution of Complex Slopes in the Three Gorges of Changjiang River. Hydrogeology and Engineering Geology, 32(1): 1-6 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SWDG200501001.htm
[8]	Ma, Y.F., Li, C.A., Wang, Q.L., et al., 2007. Statistics of Gravels from a Bore in Zhoulao Town, Jianghan Plain and Its Relationship with Cut-Through of the Yangtze Three Gorges, China. Geological Science and Technology Information, 26(2): 40-44. http://www.cqvip.com/QK/93477A/20072/24094697.html
[9]	Yin, K.L., Jian, W.X., Wang, Y., et al., 2005. Study on Genetic Mechanism and Control Method of Landslides in Horizontal Bedded of Wanzhou in Yangtze Three Gorges. China University of Geosciences Press, Wuhan (in Chinese).
[10]	Yuan, D.W., Mei, Y.T., Qin, X.L., et al., 1996. A Research of Regional Crustal Stability in and around the Dam Region of the Three Gorges Project on the Yangtze River. China University of Geosciences Press, Wuhan (in Chinese).
[11]	Zhou, F.Q., Tang, C.S., 2008. The Yangtze River Sediment Source and Accumulation Rule Research. Changjiang Press, Wuhan (in Chinese).
[12]	蔡耀军, 王军怀, 朱云发, 等, 2010. 金沙江石鼓－虎跳峡河段演化史及形成环境研究. 资源环境与工程, 24(3): 283-286. doi: 10.3969/j.issn.1671-1211.2010.03.016
[13]	陈国金, 陈松, 蹇佳洲, 2005. 水库型和降雨型滑坡地下水作用研究. 见: 湖北省三峡库区地质灾害防治工程论文集. 武汉: 湖北人民出版社.
[14]	陈松, 陈国金, 徐光黎, 2008. 黄土坡滑坡形成与变形的地质过程机制. 地球科学——中国地质大学学报, 33(3): 411-415. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200803018.htm
[15]	邓清禄, 2000. 斜坡变形构造——巴东新县城斜坡剖析. 武汉: 中国地质大学出版社.
[16]	李长安, 1997a. 地文期、构造―气候耦合与地质灾害. 地学前缘, 4(3-4): 204. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY7Z2.035.htm
[17]	李长安, 1997b. 三峡地区滑坡与构造运动、气候变化的关系. 地质科技情报, 16(3): 88-91. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ703.018.htm
[18]	刘传正, 2005. 长江三峡复杂斜坡成因问题. 水文地质工程地质, 32(1): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG200501001.htm
[19]	马永法, 李长安, 王秋良, 等, 2007. 江汉平原周老镇钻孔砾石统计及其与长江三峡贯通的关系. 地质科技情报, 26(2): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200702007.htm
[20]	殷坤龙, 简文星, 汪洋, 等, 2005. 三峡库区万州区近水平地层滑坡成因机制与防治工程研究. 武汉: 中国地质大学出版社.
[21]	袁登维, 梅应堂, 秦兴黎, 等, 1996. 长江三峡工程坝区及外围地壳稳定性研究. 武汉: 中国地质大学出版社, 14-16, 80-81.
[22]	周凤琴, 唐从胜, 2008. 长江泥沙来源与沉积规律研究. 武汉: 长江出版社, 422-423.