中国地质2013，Vol.40Issue(4)：1307-1313,7.
柴达木盆地西部地区古—始新世残-坡积物的判别及意义
Identification and significance of the Paleocene-Eocene residual-slope sediments in western Qaidam Basin
摘要
Abstract
The Cenozoic Qaidam Basin has complex sedimentary characteristics,rapid transition of sedimentary facies and various types of lithology.The authors made a systematic analysis of the lithologic characteristics of the overlying strata of the bedrock in the North Kunlun step-fault zone from geological background,core characteristics and microscopic characteristics,and concluded that the sediments are residual-slope sediments.The new understanding of the residual-slope sediments has added a new type of oil and gas reservoirs for oil and gas exploration in the Qaidam Basin and pointed out a new direction for oil and gas exploration of the overlying strata in the bedrock of Qaidam Basin.关键词
柴达木盆地/古—始新世/残积物/坡积物/判识Key words
Qaidam Basin/ Paleocene-Eocene / residual sediments / slope sediments /judgment分类
天文与地球科学引用本文复制引用
王艳清,李森明,田翔,杨体源..柴达木盆地西部地区古—始新世残-坡积物的判别及意义[J].中国地质,2013,40(4):1307-1313,7.基金项目
中国石油天然气股份有限公司重大科技专项"柴达木盆地建设千万吨油气田综合配套技术研究"子课题"柴达木盆地基础地质深化研究与战略选区"(2011E-0303)资助. （2011E-0303）
