[1]李乾坤,徐则民,张家明,等.永胜金沙江寨子村古滑坡和古堰塞湖的发现[J].山地学报,2011,(06):729.
 LI Qiankun,XU Zemin,Zhang Jiaming.The Ancient Iandslide and Dammed Lake Found in the Jinsha River near Zhaizicun, Yongsheng, Yunnan, China[J].Mountain Research,2011,(06):729.
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永胜金沙江寨子村古滑坡和古堰塞湖的发现()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2011年06期
页码:
729
栏目:
山地学报
出版日期:
2011-01-01

文章信息/Info

Title:
The Ancient Iandslide and Dammed Lake Found in the Jinsha River near Zhaizicun, Yongsheng, Yunnan, China
作者:
李乾坤;徐则民;张家明;
昆明理工大学,云南 昆明 650500
Author(s):
LI Qiankun XU Zemin Zhang Jiaming
Kunming University of Science and Technology, Kunming 650500, China
关键词:
寨子村古滑坡滑坡坝古堰塞湖堰塞湖沉积程海断裂地震
Keywords:
Zhaizicun ancient landslide landslide dam landslidedammed lake deposits of landslidedammed lake Chenghai fault earthquake
分类号:
P642.22, P941.78
文献标志码:
A
摘要:
在滇西北地区永胜南部金沙江的右岸,发现了总方量为2.5×108 m3的超大型古滑坡。滑坡后缘及两侧断壁为近直立的石灰岩峭壁,高5~30 m。滑床发育有规模不一的冲沟,覆盖有发育植被的坡积物、倒石堆和巨石。该滑坡曾造成过严重的堵江事件,在金沙江左岸仍然可以看到垄岗状残留滑坡坝,坝体方量约180×104 m3,滑坡坝和坝体后侧基岩界限清晰,两者之间岩性区别较大。滑坡堵江事件在上游形成了沿江连续分布长度约46 km的古堰塞湖沉积,沉积物主要由粉土、粉质粘土及粉细砂构成,偶夹卵石层,以水平层理为主,粉细砂层中见有小型交错层理,湖相沉积特征显著,而沉积物的树枝状平面分布进一步证实其形成于堰塞湖环境。
Abstract:
In the southern Yongsheng, the right bank of the Jinsha River and found that the total amount of square 2.5 × 108 m3 of large ancient landslide, Northwest Yunnan. The main and minor scarp that is limestone cliffs with a height of 5~30 m. In the sliding bed development of varying scale gullies, and covered by the slope sediments with vegetation, talus and separate giant rock. The landslide once dammed Jinsha river, and on the left bank can still see the raised residue landslide dam, and the dam is about 180 × 104 m3. There have a clear boundaries between the landslide dam and rear bedrock, the lithology is also a great difference between them. The events of landslides blocked river formed a continuous distribution ancient lake deposits along the length of 46 km in the upstream. sediments composed by the silt, silty clay and fine sand, occasionally with gravel layer. Sediments mainly horizontal bedding. Finesandy, ripple crosslaminated and crossstratified beds show the existence of bottom currents in the landslidedammed lake. The surface sediment distribution of dendritic further confirmed its formation in the lake environment.

相似文献/References:

[1]李天池,吴积善,R.L.舒斯特.美国西部滑坡坝的合作研究[J].山地学报,1988,(04):193.
[2]刘惠军,段志刚,崔银祥,等.植物特征与某滑坡坝形成时间和稳定性关系[J].山地学报,2003,(06):736.
[3]刘惠军,沈军辉,聂德新,等.5·12汶川地震青川县木鱼镇滑坡坝稳定性分析[J].山地学报,2008,(03):263.

备注/Memo

备注/Memo:
收稿日期(Received date):2011-03-11;改回日期(Accepted) : 2011-09-10。
基金项目(Foundation item):国家自然科学基金-云南联合基金重点项目(U1033601)和国家自然科学基金 (40572159, 40772189)。\[National Natural Science Foundation Project-Key Project of Yunnan Union Foundation (U1033601) and National Natural Science Foundation Project(40572159, 40772189).\]
作者简介(Biography):李乾坤(1985–),男,江苏徐州人,硕士研究生,地质工程专业,主要从事灾害地质与环境地质研究。 \[Li Qiankun (1985-), male, born in Xuzhou, Jiangsu, Geological Engineering, majoring in the hazard geological and environment geology.\] Tel:15198907330,E-mail:lqkxxx@163.com
更新日期/Last Update: 1900-01-01