STUDY ON THE TRANSPORT PATH OF PALEO-PROVENANCE IN THE SECOND MEMBER OF SHAHEJIE FORMATION IN SHENGTUO AREA, DONGYING DEPRESSION

SUN Qi-chen; YANG Jun-sheng

2019 Vol. 28, No. 1

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SUN Qi-chen, YANG Jun-sheng. STUDY ON THE TRANSPORT PATH OF PALEO-PROVENANCE IN THE SECOND MEMBER OF SHAHEJIE FORMATION IN SHENGTUO AREA, DONGYING DEPRESSION[J]. Geology and Resources, 2019, 28(1): 43-48.

Citation:

SUN Qi-chen, YANG Jun-sheng. STUDY ON THE TRANSPORT PATH OF PALEO-PROVENANCE IN THE SECOND MEMBER OF SHAHEJIE FORMATION IN SHENGTUO AREA, DONGYING DEPRESSION[J]. Geology and Resources, 2019, 28(1): 43-48.

STUDY ON THE TRANSPORT PATH OF PALEO-PROVENANCE IN THE SECOND MEMBER OF SHAHEJIE FORMATION IN SHENGTUO AREA, DONGYING DEPRESSION

School of Earth Sciences and Technology, China University of Petroleum, Qingdao 266000, Shandong Province, China

Received Date: 30 March 2018

Revised Date: 11 June 2018

Publish Date: 28 February 2019

Abstract

Abstract

According to the stratigraphic correlation and thickness maps by drilling and logging data from over 330 wells, the paper establishes stratigraphic framework to reveal its development, and shows the distribution of sandbody deposits with sandstone thickness and percentage content. The results show that during the sedimentary period of Upper Es₂ in Shengtuo Oilfield, there are three major provenances and one secondary provenance. The distribution of sandstone thickness in each sublayer reveals the distribution of internal provenances. The provenance in different sand formations or sublayers constantly migrate within a certain area, and the transportation directions of detrital materials in the basin also change correspondingly, which leads to the superimposition of sediments from provenances of different periods and sublayers. The synsedimentary faults also affect the provenance, and the strike controls the stratigraphic distribution and transport direction of detrital materials in the study area.
- upper Es₂ /
- source direction /
- transport path /
- detrital material /
- Dongying Depression /
- Shandong Province

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References

[1]	吴伟, 杨圣贤, 刘文业, 等.胜坨油田勘探开发50年实践与认识——油藏地质篇[M].北京:石油工业出版社, 2013:173-175. Google Scholar
[2]	杨仁超, 李进步, 樊爱萍, 等.陆源沉积岩物源分析研究进展与发展趋势[J].沉积学报, 2013, 31(1):99-107. Google Scholar
[3]	胜利油田有限公司胜利采油厂编写.胜坨地区沙二段三角洲前缘砂体分布及含油气规律研究[M].北京:石油工业出版社, 2003:17-20. Google Scholar
[4]	林畅松, 郑和荣, 任建业, 等.渤海湾盆地东营、沾化凹陷早第三纪同沉积断裂作用对沉积充填的控制[J].中国科学:D辑(地球科学), 2003, 33(11):1025-1036. Google Scholar
[5]	孙永壮.东营凹陷胜坨地区沙河街组沉积体系及其油气源特征[J].中国石油大学学报:自然科学版, 2006, 30(06):24-30. Google Scholar
[6]	胜利油田石油地质志编写组.中国石油地质志(卷六)[M].北京:石油工业出版社, 1993:20-25. Google Scholar
[7]	柯光明, 郑荣才, 高红灿, 等.胜坨油田一区沙河街组二段1-3砂组测井-沉积相分析[J].沉积与特提斯地质, 2006, 26(1):81-87. Google Scholar
[8]	王风华.东营凹陷东北斜坡带沉积特征及成藏规律研究[J].断块油气田, 2004, 11(2):8-9. Google Scholar
[9]	彭治超, 付星辉, 刘俊超, 等.沉积物源分析方法及研究进展[J].西安文理学院学报:自然科学版, 2017, 20(1):116-121. Google Scholar
[10]	仲虹.地球化学在物源及沉积背景分析中的应用[J].智能城市, 2017, 3(12):183. Google Scholar
[11]	魏然, 李红阳, 于斌, 等.沉积盆地物源体系分析方法及研究进展[J].岩性油藏, 2013, 25(3):53-57. Google Scholar
[12]	张立强, 杨晚.东营凹陷北带古冲沟古近系多物源沉积模式[J].中南大学学报:自然科学版, 2012, 43(8):3159-3165. Google Scholar
[13]	赖维成, 宋章强, 周心怀, 等."动态物源"控砂模式[J].石油勘探与开发, 2010, 37(6):763-768. Google Scholar
[14]	王秀红.渤海湾盆地沾化凹陷富林洼陷油气来源及分布规律研究[J].石油实验地质, 2013, 35(2):151-156. Google Scholar
[15]	曹翠.胜坨油田一区沙河街组二段1~3砂组构造精细研究[J].西部探矿工程, 2010, 22(12):25-28. Google Scholar