[1]崔之久,张梅,崔鹏,等.初论堰塞湖溃坝沉积相特征[J].山地学报,2015,(02):129.
　CUI Zhijiu,ZHANG Mei,et al.Discussion on Characteristics of Sedimentary Facies of Dammedlakes Outburst Deposits[J].Mountain Research,2015,(02):129.
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初论堰塞湖溃坝沉积相特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年02期
页码:
129
栏目:
山地环境
出版日期:
2015-04-01

文章信息/Info

Title:
Discussion on Characteristics of Sedimentary Facies of Dammedlakes Outburst Deposits
作者:
崔之久;张梅;崔鹏;陈剑;魏明建;葛永刚;陈艺鑫;李川川;
北京大学城市与环境学院;北京大学深圳研究生院;北京师范大学环境演变与自然灾害教育部重点实验室;中国科学院水利部成都山地灾害与环境研究所;中国地质大学(北京)工程技术学院;首都师范大学资源环境与旅游学院;
Author(s):
CUI Zhijiu; ZHANG Mei; CUI Peng; CHEN Jian; WEI Mingjian; CHEN Yixin; LI Chuanchuan
1.College of Urban and Environmental Sciences,Peking University, Beijing 100871, China; 2.Shenzhen Graduate School,Peking University, Shenzhen 518055, China; 3.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China; 4.School of Engineering and Technology,China University of Geosciences, Beijing 100083, China; 5.College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China
关键词:
溃坝堆积; 冰川-冰碛; 火山堆积; 块体运动堆积; 混杂堆积
Keywords:
dammedlakes outburst deposits; glouiermoranes; Volcanic pile; block movement accumulation; confoundingdeposits
分类号:
P512.2，P931
文献标志码:
A
摘要:
堰塞湖溃坝类型包括冰川、冰碛,火山和多种块体地貌(滑坡、崩塌、泥石流等)过程,而溃坝堆积相的种种特点以后者所造成的最具代表性。堆积体平面展布范围大(几平方公里~几十平方公里),剖面规模也大(高几十米),层次(层理)和结构全剖面均一,无超大的砾石;微观上有部分泥石流堆积特点,显示是高密度流,搬运介质是水。堆积体很少细砂和粘土物质。在平面上可划分出:扇顶(上游)、扇中(中游)、扇缘(下游)等微相。
Abstract:
According to their dam modes of origin, dammedlakes outburst deposits can be devided into glacierdammedlakes and morainedammedlakes, lavadammedlakes and mass movements (landslide, collapse, debris flow)- dammedlakes. Furthermore, characteristics of sedimentary facies which are caused by mass movements are most representative. Our preliminary research and reference to others’ work on mass movementsdammedlakes outburst deposits of several typical regions (Xuelongnang, Yinchanggou, Tangjiashan and the source region of Minjiang) demonstrate that spreading areas of many accumulated body are enormous ranging from several square kilometers to dozens of square kilometers; section sizes are also massive with heights of dozens of meters; layers (beddings) and structures in the whole profile are homogeneous without oversized gravels. Microscopically, certain features of accumulated body are similar to debris flow such as current of higher density with water as transporting media. Microfacies of accumulation body can be divided into fanhead (upstream), middle fan (midstream) and fan fringe (downstream).

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备注/Memo

备注/Memo:
收稿日期(Received date)：2013-12-19；改回日期(Accepted) : 2014-06-05。
基金项目（Foundation item）：国家自然科学基金重点项目(41230743)。[Key Program of National Natural Science Foundation of China (41230743).]
作者简介（Biography）：崔之久（1933-），男，教授，主要从事混杂堆积与第四纪冰川方面的研究。[Cui Zhijiu(1933-), male, professor, specialized in diamiction and quaternary glaciation.] E-mail:czj@urban.pku.edu.cn *
通信作者(Corresponding author)：张梅（1985-），女，博士，主要从事地貌学与第四纪环境研究。[Zhang Mei (1985-), female, Ph D, major in study of geomorphology and quaternary environment.] E-mail:jluzhangmei@163.com
更新日期/Last Update: 1900-01-01