干旱区生态环境知识资源中心(Arid): 东昆仑库木库里沙漠表层沉积物粒度特征、物源与沉积环境

Arid

	东昆仑库木库里沙漠表层沉积物粒度特征、物源与沉积环境
其他题名	Grain-size characteristics,provenance discrimination and sedimentary environment of the surface sediments from Kumkol Desert of Eastern Kunlun Mountain
	凌智永 1; 周亚辉 2; 李廷伟 1; 马海州 1; 李建森 1
来源期刊	干旱区地理
ISSN	1000-6060
出版年	2017
卷号	40 期号:5 页码:1013-1019
中文摘要	对青藏高原北部世界海拔最高的库木库里沙漠周围冲积扇碎屑及沙漠表层沉积物粒度特征及元素组成研究结果显示:(1)库木库里沙漠表层沉积物以细砂为主,其次为极细砂,粉砂和中砂含量较少,有少量的黏粒,不含粗砂的组分,且粒度组成差异不大。(2)沉积物MZ范围2.70~ 2.90 Ф,sigma_1范围0.80~1.10 Ф,S_(K1)范围0.26~0.44,KG范围2.27~3.62。(3)粒度主要呈近似对称的单峰分布,但细颗粒一侧有较细长的尾部。(4)沙漠表层沉积物元素组成与周围山麓冲洪积碎屑沉积物较为相似,尤其是沙漠西部的阿尔喀山北麓区域。(5)沉积物源判别表明,沙漠表层沉积物来源主要为阿尔喀山北麓及祁漫塔格山南麓碎屑沉积物,其形成环境主要为河流相沉积环境及浅湖相沉积环境。
英文摘要	The study of grain size and geochemical elements composition of sediments are very important to distinguish their sedimentary environment,dynamic conditions of transporting,migration patterns and material sources. Field survey,sampling,laboratory experiment and other methods were used in this paper. A total of 32 samples of surface sediments from different regions in the world’s highest altitude desert,Kumkol Desert,on the northern Qinghai-Tibetan Plateau,were analyzed in the lab to analyze the grain size characteristics,geochemical elements composition and the elements composition of the alluvial- fan clastic. The results showed as follows: (1)Surface sediments from Kumkol Desert are mainly silver sand,its content is about 60%. There is a certain amount of very fine sand,the content of silty sand and medium sand is little and closed. A small amount of clay was contained,but excluding coarse sand component and the grain size composition is very similar. Frequency curves of grain size are the approximate symmetrical unimodal distribution,but the left side has a long tail comprised by the fine grain size which are greater than 4 Ф(<0.063 mm),and are mainly the silty and clay components.(2)The MZ range of the dunes surface sediments is 2.70-2.90 Ф and mean value is 2.79 Ф. The MZ range of the field among the dunes is 2.80-2.86 Ф and mean value is 2.83 Ф. The range of sigma_1 are 0.80-1.10Ф and 0.93- 1.10 Ф,the mean value are 1.01 Ф and 1.03 Ф,sorting is middling. The range of S_(K1) are 0.26-0.44 and 0.35-0.41, the mean value are 0.37,and kurtosis is positive. The range of KG are 2.27-3.62 and 2.80-3.01,the mean value are 2.95,2.93,and kurtosis is a single peak.(3)The geochemical elements of desert surface sediment and the alluvial clastic sediment from surrounding piedmont are similar,especially similar to the north area of Aerka Mountain in the western desert.(4)The analyzed sources of the sediment reveal that the desert surface sediment is mainly from the north area of Aerka Mountain and the south area of Qimantage Mountain,and its formation environment is mainly fluvial facies sedimentation and shallow lacustrine facies sedimentation. Since the Kumkol Desert has been formed for no long time,the sediment still shows a good inheritance to its sources. Those preliminary results have important significance for developing a comprehensive index to distinguish the sedimentary environment, dynamic conditions of transporting,migration patterns and material sources of the sediments and show the interaction between aeolian and fluvial processes in Kumkol Desert. In short,the research of Kumkol Desert,can not only reveal its cause and evolution characteristics,but also help us to understand the surrounding environment of the Kumkol Basin and the climate changes of the Qinghai-Tibetan Plateau. At the same time,the study can also extend the distribution scope of desert research area in China,to some extent,desert research of regional imbalance can be changed.
中文关键词	表层沉积物 ; 粒度特征 ; 物源判别 ; 沉积环境 ; 库木库里沙漠
英文关键词	surface sediment characteristic of grain size provenance discrimination sedimentary environment Kumkol Desert
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向	Geology
CSCD记录号	CSCD:6101139
来源机构	中国科学院西北生态环境资源研究院
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/235950
作者单位	1.中国科学院青海盐湖研究所, 西宁, 青海 810008, 中国; 2.甘肃省地质调查院, 兰州, 甘肃 730000, 中国
推荐引用方式 GB/T 7714	凌智永,周亚辉,李廷伟,等. 东昆仑库木库里沙漠表层沉积物粒度特征、物源与沉积环境[J]. 中国科学院西北生态环境资源研究院,2017,40(5):1013-1019.
APA	凌智永,周亚辉,李廷伟,马海州,&李建森.(2017).东昆仑库木库里沙漠表层沉积物粒度特征、物源与沉积环境.干旱区地理,40(5),1013-1019.
MLA	凌智永,et al."东昆仑库木库里沙漠表层沉积物粒度特征、物源与沉积环境".干旱区地理 40.5(2017):1013-1019.