成都理工大学学报（自然科学版）Issue(1)：77-85,9.DOI:10.3969/j.issn.1671-9727.2016.01.08
痕量元素和碳氧同位素在塔里木盆地西南缘棋盘组沉积环境研究中的应用
Application of trace elements and carbon-oxygen isotopes on the research of sedimentary environment of the Qipan Formation in the southwest margin of Tarim Basin,China
摘要
Abstract
Qipan Formation formed in a high salinity on shore marine sedimentary environment with a warm to dry climate,and in poor oxygen to anaerobic environment favorable to the enrichment of organic matter.It considers that the trace elements and carbon-oxygen isotopes parameters are closely related to the sea-level changes.The Qipan Formation shows a regressive to transgressive process with four sub-cycles,and the variation of sea-level results in the frequent occurrence of interbeds of mudstone and bioclastic limestone in Qipan Formation.关键词
痕量元素/碳氧同位素/沉积环境/塔里木盆地/棋盘组Key words
trace elements/carbon-oxygen isotopes/sedimentary environment/Tarim Basin/Qipan Formation分类
天文与地球科学引用本文复制引用
孟苗苗,康志宏,樊太亮,冯晓利,童雪飞,于超..痕量元素和碳氧同位素在塔里木盆地西南缘棋盘组沉积环境研究中的应用[J].成都理工大学学报（自然科学版）,2016,(1):77-85,9.基金项目
全国油气资源战略选区调查与评价国家专项（第二批）（2009GYXQ02）。 （）
