[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 ZhijiuZHANG MeiCUI PengCHEN JianWEI MingjianCHEN YixinLI 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
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。

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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