Grain Size Variation of Quaternary Sediments Related to Paleoclimate Change in Tarim Basin,Northwest China

机译：塔里木盆地古气候变化与第四纪沉积物粒度变化

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INTRODUCTION Quaternary sediments contain the records related to the changes in paleoclimate and paleoenvironment. Grain size of the sediments is taken as the good indicator of the sedimentary environmental conditions related to the climate change (Xiao et al., 1995; McLaren and Bowles, 1985; Glasiter and Nelson, 1975). We report here the data of KT2 core samples to show the change of Quaternary paleoclimate in Tarim basin in Northwest China. BH KT2 core is located at the hinterland of Tarim basin (Fig. 1) and covers the whole Quaternary strata. The grain size was measured by Mastersizer-2000 Laser Grain Size Analyzer in the Laboratory of Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences.

机译：引言第四纪沉积物包含与古气候和古环境变化有关的记录。沉积物的粒度被视为与气候变化有关的沉积环境条件的良好指标（Xiao等，1995； McLaren和Bowles，1985； Glasterr和Nelson，1975）。我们在此报告KT2岩心样品的数据，以显示中国西北塔里木盆地第四纪古气候的变化。 BH KT2岩心位于塔里木盆地腹地（图1），覆盖整个第四纪地层。用中国地质科学院水文地质与环境地质研究所实验室的Mastersizer-2000激光粒度分析仪测量粒度。

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《The International Conference of Geobiology(地球生物学国际研讨会）》|2010年|p.257-259|共3页
会议地点 Wuhan(CN)
作者
Song Shuhong; Bi Zhiwei; Yang jing; Yang Zhenjing;
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School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Shijiazhuang 050061, China;

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Shijiazhuang 050061, China;

School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences,Shijiazhuang 050061, China;

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Grain Size Variation of Quaternary Sediments Related to Paleoclimate Change in Tarim Basin,Northwest China

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