鄂尔多斯盆地长7 段浊积岩沉积演化模式及石油地质意义
网络出版日期: 2009-12-16
基金资助
国家重点基金研究发展计划项目(编号:2003CB214602)与长江学者和创新团队发展计划(编号:IRT0559)联合资助
Sedimentary evolution model and petroleum significance of Chang-7 member turbidite,Ordos Basin
Online published: 2009-12-16
高长海 , 查明 . 鄂尔多斯盆地长7 段浊积岩沉积演化模式及石油地质意义[J]. 岩性油气藏, 2009 , 21(4) : 73 -77 . DOI: 10.3969/j.issn.1673-8926.2009.04.014
The extensive extent turbidite can be identified by such apparent signatures as lithology, sedimentary structure, sedimentary sequence and well logs ofChang-7 member deep lake, Ordos Basin. During the paleo-geographic evolution of Chang-7 member, lake basin and deep lake are both at their maximum extent during Chang-73 stage, and turbidite was distributed fragmental-like in plane view, due to interplay of extensive extent deep lake and limited clastic supplying. Deep lake line was graduallymoved toward lake center and turbidite sand bodies were gradually developed better from stages of Chang-73, Chang-72 and Chang-71. And depositional evolution model in study area is established. There is better petroleum accumulation in deep lake, and turbidite sandstone can be better reservoir in deep lake. At present, some commercial oil wells were found in Southwest Ordos Basin and the turbidite sandstones can be the main exploration targets in the near future.
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