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鄂尔多斯志丹地区延长组高分辨率层序地层模式探讨
引用本文:周林,陈波,赵进义,慕丹,周坤.鄂尔多斯志丹地区延长组高分辨率层序地层模式探讨[J].科学技术与工程,2014,14(1).
作者姓名:周林  陈波  赵进义  慕丹  周坤
作者单位:长江大学地球科学学院;长江大学湖北省非常规油气协同创新中心,长江大学地球科学学院;长江大学湖北省非常规油气协同创新中心,延长油田股份有限公司,延长油田股份有限公司,西南石油大学资源与环境学院
摘    要:根据岩心、野外露头、测井、录井岩性等资料,在高分辨率层序地层学理论体系的指导下,按照适合陆相盆地层序特征的研究思路,对鄂尔多斯盆地陕北斜坡带志丹地区延长组地层特征进行了研究。对志丹地区延长组不同相带、不同旋回中岩性组合特征进行分析,总结出了该地区延长组层序界面的类型和识别特征;并对延长组基准面旋回特征进行讨论和长期基准面旋回的划分。最后在此基础上提出志丹地区延长组长10—长4+5时期的高分辨率层序地层模式。认为延长组从下至上可以划分为四个长期基准面旋回,其中LSC1对应长10和长9油组;LSC2对应长8和长7油组;LSC3对应长6和长4+5油组;LSC4对应长3、长2和长1油组。LSC3生储盖组合配置良好,且处于油气运移的有利指向上,是志丹地区主要的产油层段。

关 键 词:高分辨率层序地层  长期基准面旋回  鄂尔多斯盆地延长组  层序地层界面  志丹地区
收稿时间:2013/7/12 0:00:00
修稿时间:2013/7/12 0:00:00

The Discussion of the High-Resolution Sequence Stratigraphy Models of Yanchang Formation in Zhidan Area of Ordos Basin
Zhoulin,Chenbo,Zhaojinyi,Mudan and Zhoukun.The Discussion of the High-Resolution Sequence Stratigraphy Models of Yanchang Formation in Zhidan Area of Ordos Basin[J].Science Technology and Engineering,2014,14(1).
Authors:Zhoulin  Chenbo  Zhaojinyi  Mudan and Zhoukun
Abstract:According to the information of drilling core,field outcrop, logging curves,lithologic combination etc, under the guidance of the high resolution sequence stratigraphy theory system, on the basis of research ideas which suitable for continental basin sequence characteristics , the paper studied the sequence stratigraphy of Yanchang Formation in Zhidan area of the Shanbei slope in Ordos Basin. The paper analysed the lithologic characters of of Yanchang Formation in Zhidan area with different facies and circles, summarized the type of high resolution sequence stratigraphy interface and the recognition features in Zhidan area, divided the long-term stratigraphic base-level circles of Yanchang Formation and analyzed the characteristics of each base level cycle. Finally, on that basis, the paper put forward the high resolution sequence stratigraphic model of Yanchang Formation in Zhidan area during the time between Chang10 and Chang4+5. The paper concluded that Yanchang Formation can be divided into four long-term base-level cycles from the bottom to the top. And LSC1 is correspond with Chang10 oil layer and Chang9 oil layer, LSC2 is correspond with Chang8 oil layer and Chang7 oil layer, LSC3 is correspond with Chang6 oil layer and Chang4+5 oil layer, LSC4 is correspond with Chang3 oil layer ,Chang2 oil layer and Chang1 oil layer. With a good source-reservoir-caprock association , located in a favorable direction of oil and gas accumulation, LSC3 was the main oil producing interval of Zhidan area.
Keywords:high resolution sequence stratigraphy  long-term stratigraphic base-level circles  Yanchang Formation  Ordos Basin  sequence stratigraphy interface  Zhidan area
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