GROWTH HISTORY OF HUANGTUPO LANDSLIDE: DOWN-SLOPE OVERLAPPING-LANDSLIDING-MODIFICATION
-
摘要: 长江三峡库区巴东新县城黄土坡是否为古滑坡、滑坡的范围有多大、新滑坡与古滑坡的关系如何等, 还存在着不同认识.基于大量的野外观察资料, 提出了坠覆-滑坡-改造多阶段变形、失稳的斜坡演化模式.认为黄土坡在滑坡以前经历了长期的坠覆作用, 坠覆包括了倾倒和深层蠕变两种基本的斜坡变形型式; 坠覆的基础上发生了滑坡, 造成了台阶状地貌、构造面线与基岩不协调及滑动角砾岩带等现象; 滑坡形成后受水文、地貌等条件的影响, 长期经历着小规模滑坡的叠加改造, 1995年发生的两次滑坡仍是进一步改造的结果.黄土坡坠覆-滑坡-改造这一有机联系的岩质斜坡变形过程的建立, 使得关于黄土坡的一些重大问题有了比较明确的认识, 这也为构造学解决斜坡研究中的一些问题提供了一个典范.Abstract: In 1995 two landslidesin the Huangtupo slope in the Three Gorges Reservoir region turned into a hot issue among the engineering geologists and the Chinese government.Although many researches have been made into the slope, there are still many controversiesover the characteristicsof the Huangtupo slope. Is the Huangtupo slope in the new county of Badong, Three Gorges Reservoir region an ancient landslide? If so, what was the scale of this ancient landslide? What is the relationship between the new landslides and the old landslides? The present paper proposes, on the basis of a great number of field observation references, the slope evolutionary pattern of deformation and instability in the multi_stages of down_slope overlapping, lands-liding, and modification. Before the landslide, the Huangtupo slope experienced the long_term down_slope overlapping classified as included toppling and deep_seated creeping, two basic slope deformation forms. The Huangtupo landslide, derived from the preceding down_slope overlapping, brought about the step_like land-form. The significant evidences for the landslide are the varied attitudesof structural surfaces and linesof out-crops in the slope and the presence of the sliding breccia zones.Since then, the Huangtupo landslide hasexpe-rienced small_scale overlapping modifications of landslides. The two landslides that occurred in 1995 were the result of the further modification. It is concluded that the rock slope deformation process of down_slope over-lapping_landsliding_modification is an organic one. This conclusion presents us with relatively precise under-standing of some important issues about the Huangtupo landslide and also with a typical example of the appli-cation of the tectonics to the research into slopes.
-
图 2 黄土坡变形斜坡地质略图
1.巴东组第三段泥质灰岩; 2.巴东组第二段泥质粉沙岩及粉沙质泥岩; 3.松散的块石土堆积中的岩块露头(其岩层产状和劈理产状标在旁侧); 4.坠覆改造区; 5.滑坡边界; 6.黄土坡小范围滑坡的前端边界; 7.坠覆与基岩的过渡边界; 8.岩层产状; 9.劈理产状; 10.直立劈理; ①二道沟滑坡; ②三道沟西侧滑坡
Fig. 2. Geological sketch map of Huangtupo slope
图 3 黄土坡滑坡前缘滑带(图例同图 2)
a.四道沟口东300 m; b.二道沟口西200 m
Fig. 3. Sliding zone in the front edge of Huangtupo landslide
-
[1] 吴永锋. 黄土坡滑坡及其主要地质问题[A]. 见: 崔政权编. 岩土工程论文集[C]. 武汉: 中国地质大学出版社, 1996.93-97. [2] 钟立勋, 殷跃平, 唐灿. 三峡工程库区拟迁城市巴东县新城址环境地质研究[A]. 见: 地质矿产部环境地质研究所. 地质矿产部环境地质研究所论文集: 第一集[C]. 北京: 地质出版社, 1992.41-53. [3] Nemcok A. Gravitational slope deformation in high mountains [A]. Proceedings 24 Int Geological Congress[C]. Montreal. 1972, Sect. 13: 132-141. [4] Hutchinson J N. Mass movement [A]. In: Fairbridge R W, ed. Encyclopedia Geomorphology[C]. New York: Reinhold, 1968.688-696. [5] Mahr T. Deep reaching gravitational deformations of high mountain slopes[J]. Engineering Geology, 1977, 16: 121-127. [6] 晏同珍. 水文工程地质与环境保护[M]. 武汉: 中国地质大学出版社, 1994.41-42. [7] Chigira M. Long_term gravitational deformation of rocks by mass rock creep[J]. Engineering Geology, 1992, 32: 157-184. doi: 10.1016/0013-7952(92)90043-X [8] 邓清禄, 王学平. 斜坡深层岩石蠕变与黄土坡滑坡[J]. 长春科技大学学报, 1999, 29 (1): 60-63. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ901.012.htm [9] 喻学文, 吴永锋. 长江三峡巴东县城区三道沟滑坡成因研究[J]. 工程地质学报, 1996, 4 (1): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-GCDZ601.000.htm [10] 邓清禄. 长江三峡库区巴东新县城构造与斜坡稳定性研究[D]. 武汉: 中国地质大学, 1998. -
下载:
点击查看大图
图(5)
计量
- 文章访问数: 3727
- HTML全文浏览量: 132
- PDF下载量: 8
- 被引次数: 0
