[1]崔之久,冯金良.东川蒋家沟泥石流沉积亚相组合特征[J].水土保持研究,2001,8(02):2-6.
　CUI Zhi-jiu,FENG Jin-liang.Combination Features of Depositional Sub-facies of Debris-flowon the Jiangjiagou Valley, Yunnan Province[J].Research of Soil and Water Conservation,2001,8(02):2-6.
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东川蒋家沟泥石流沉积亚相组合特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 8 期数: 2001年02期 页码: 2-6 栏目: 出版日期: 1900-01-01
Title:
Combination Features of Depositional Sub-facies of Debris-flowon the Jiangjiagou Valley, Yunnan Province
作者:
崔之久1, 冯金良1,2
1. 北京大学城市与环境学系, 北京, 100871;
2. 河北省科学院地理研究所, 石家庄, 050011
Author(s):
CUI Zhi-jiu1, FENG Jin-liang1,2
1. Department of Urban and Environmental Sciences, Peking University, Beijing, 100871, China;
2. The Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011
关键词:
蒋家沟; 泥石流; 沉积亚相; 夷平面解体
Keywords:
Jiangjiagou valley; debris flow; depositional sub facies; deformation of the planation surface
分类号:
P642.23
摘要:
在自然界中,泥石流形成环境、发育规律、空间分布等特征的演化和分异,导致了不同时期、不同区域、不同沉积过程和不同沉积地貌部位泥石流沉积亚相组合的变异.该文拟在作者所建泥石流沉积模式基础上,以蒋家沟为例进一步讨论泥石流亚相的组合及变异规律.此外,初步探讨了夷平面解体后,泥石流沉积在地貌回春不同阶段的发育规律.
Abstract:
In the nature,due to the debris flow developing under different environment and depositing various landform,it led to combination variation of depositional sub facies on the different period,various regions and different depositional landform.On the basis of depositional model of debris flow built by author,the combination and variation of depositional sub facies of debris flow on the Jiangjiagou valley,Yunnan Province,was discussed.The main features of debris flow of Jiangjiagou are as follows:(1)the erosion layer(C) very developed;(2)the layer(B) of surface mud didn’t run in succession;(3)the thickness of debris layer(A) is thin;(4)the layer(D) of floor mud developed weakly.The main combination of sub facies is C-A-C and B-A-C.

参考文献/References:

[1] 施雅风,崔之久,李吉均,等.中国东部第四纪冰川与环境问题[M].北京:科学出版社,1989.26～62.
[2] 崔之久,等.泥石流沉积与环境[M].北京:海洋出版社,1996.46～57.
[3] 杜榕桓,康志成,陈循谦,等.云南小江流域泥石流综合考察与防治规划研究[M].重庆:科学技术文献出版社重庆分社,1987.249～254.
[4] 吴积善,等.云南蒋家沟泥石流观测研究[M].北京:科学出版社,1990.
[5] 周必凡,等.泥石流防治指南[M].北京:科学出版社,1991.
[6] 崔之久.沟谷泥石流及扇形地的沉积类型与形成机制[J].沉积学报,1986,3(2):69～79.
[7] 崔之久,熊黑钢.泥石流沉积相模式[J].沉积学报,1990,3(2):128～140.
[8] 何浩生,何科昭.滇西地区夷平面变形及其反映的第四纪构造运动[M].现代地质,1993,7(1):31～39.
[9] 宋方敏,等.小江活动断裂带[M].北京:地震出版社,1998.22～75.
[10] 谢又予,等.沉积地貌分析[M].北京:海洋出版社,2000.54～71.
[11] H.G.里丁.沉积环境和相[M].周明鉴等译.北京:科学出版社,1985.

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备注/Memo

收稿日期:2001-3-21。
基金项目:中国科学院东川泥石流观测站资助项目(1999-2001)
作者简介:崔之久(1933- ),男,教授,博士生导师,主要从事气候地貌与沉积等研究.

更新日期/Last Update: 1900-01-01