[1]白 雪,杨振京*,毕志伟,等.银川盆地第四纪沉积物粒度特征及其沉积环境[J].山地学报,2017,(06):874-881.[doi:10.16089/j.cnki.1008-2786.000289]
 BAI Xue,YANG Zhenjing,BI Zhiwei,et al.Grain Size Characteristics and Its Depositional Environmentof Quaternary Sediments in Yinchuan Plain, Northwest China[J].Mountain Research,2017,(06):874-881.[doi:10.16089/j.cnki.1008-2786.000289]
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银川盆地第四纪沉积物粒度特征及其沉积环境()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2017年06期
页码:
874-881
栏目:
山地灾害
出版日期:
2017-11-30

文章信息/Info

Title:
Grain Size Characteristics and Its Depositional Environment of Quaternary Sediments in Yinchuan Plain, Northwest China
文章编号:
1008-2786-(2017)6-874-08
作者:
白 雪12 杨振京1* 毕志伟1孙玉芳3刘林敬1
1.中国地质科学院 水文地质环境地质研究所,河北 正定 050803; 2.河北地质大学,河北 石家庄 050031; 3.宁夏回族自治区水文环境地质勘察院,宁夏 银川 750001
Author(s):
BAI Xue12 YANG Zhenjing1 BI Zhiwei1 SUN Yufang3 LIU Linjing1
1.Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Shijiazhuang 050803, China; 2.Hebei GEO University,Shijiazhuang 050031, China; 3.Institute of Hydrogeology and Environmental Geology of Ningxia,Yingchuan 750001, China
关键词:
第四纪 粒度 沉积环境 银川平原
Keywords:
Quaternary grain size sedimentary environment Yingchuan Plain
分类号:
P534.63
DOI:
10.16089/j.cnki.1008-2786.000289
文献标志码:
A
摘要:
本文通过对银川平原深达900米的YE07钻孔沉积物进行粒度分析,结合其他钻孔的研究资料,探讨了银川平原中更新世以来沉积环境的演化过程,发现银川平原沉积环境的变化主要受气候和构造因素的影响,其演化过程表现出一定的区域特点,主要经历了以下的演化阶段: 722 ~ 664 ka B.P.属于湖沼相沉积; 664 ~ 126 ka B.P.沉积环境以河流相沉积为主,水动力条件较强,沉积动能较高; 126 ~ 11 ka B.P.的沉积环境是以河流相为主的河湖交替相; 11 ka B.P.以来沉积环境主要表现为河湖相沉积。银川平原沉积环境的研究为其水文地质研究和第四纪地层划分提供新的理论依据。
Abstract:
Based on grain size analysis of the sediment from Borehole YE07 at the depth of 900 m in the Yinchuan Plain of Northwest China and with reference to previous data, the evolution process of depositional environment in the Yinchuan Plain was studied since the middle Pleistocene.The results indicated that the main changes of depositional environment in the study area were mainly controlled by climate, geological structures, and evolution process, which showed distinct regional characteristics underwent the following evolution stages: 1)lacustrine deposition during 722-664 ka B.P.; 2)mainly fluvial deposition during 664-126 ka B.P., with stronger hydrodynamic conditions and higher kinetic energy; 3)fluvio-lacustrine alternating deposition with the fluvial deposition as the main during 126-11 ka B.P.; and 4)mainly fluvio-lacustrine deposition since 11 ka B.P..This research provid a new theoretical foundation for the study of hydrogeology and the division of quaternary sediments in the Yinchuan Plain.

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备注/Memo

备注/Memo:
收稿日期(Received date):2016-10-22; 改回日期(Accepted date):2017-03-27
基金项目(Foundation item):中国地质调查项目(1212011220937); 中国地质科学院基本科研业务费专项经费(YYWF201627)[Project of China Geological Survey(1212011220937); Basic Scientific Research Special Funds Project of Chinese Academy of Geological Sciences(YYWF201627)]
作者简介(Biography):白雪(1992-),女,硕士研究生,主要从事构造地质与第四纪环境研究[Bai Xue, female, M.Sc.candidate, research on tectonic geology and quaternary environment] E-mail:739151325@qq.com
*通讯作者(Corresponding author):杨振京(1966-),男,研究员,主要从事第四纪地质与环境研究[Yang Zhenjing, male, professor, research on quaternary environment] E-mail: yangzhenjing1966@163.com
更新日期/Last Update: 2017-11-30