Provenance analysis of Chang 9 oil reservoir set in Longdong area, Ordos Basin

  • PAN Shaowei ,
  • LIANG Hongjun ,
  • LI Liang ,
  • LUO Haining ,
  • WANG Jiahua
Expand
  • 1. Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Xi’an 710021, China; 2. National Engineering Laboratory for Exploration and Development of Low-Permeability Oil & Gas Fields, Xi’an 710018, China; 3. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Online published: 2012-10-20

Abstract

There maybe exist multiple source supply during the sedimentation period of the Chang 9 oil reservoir set in Longdong area. Provenance analysis is not only the basis of study the delta development characteristics of Chang 9 oil reservoir set, but also the foundation for evaluation and prediction of sand bodies. Based on the relative change of quartz content, heavymineral assemblages, quartz cathodoluminescence, debris content and paleosalinity recovery, it is considered that the deposition is controlled by the sources from the southwest, the northwest, the south and the northeast of Longdong area at the same time. The southwest of the study area is the main source area, followed by the south, the northwest and the northeast. The parent rocks in the southwest are middle-high grade metamorphics and volcanics in the Qilian tectonic belt, while the source in the south, the northwest and northeast is granite and low-middle grade metamorphics fromthe Southern Qinling tectonic belt, Alaschanica ancient land and Yinshan ancient land respective. The sediments that come fromdifferent directions converge at the area ofYuancheng-Huachi-Majiabian-Taibai.

Cite this article

PAN Shaowei , LIANG Hongjun , LI Liang , LUO Haining , WANG Jiahua . Provenance analysis of Chang 9 oil reservoir set in Longdong area, Ordos Basin[J]. Lithologic Reservoirs, 2012 , 24(5) : 71 -75 . DOI: 10.3969/j.issn.1673-8926.2012.05.013

References

[1] 陈洪德,倪新锋.陇东地区三叠系延长组沉积层序及充填响应特征[J].石油与天然气地质,2006,27(2):143-151.
[2] 李凤杰,王多云,张庆龙,等.鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析[J].沉积学报,2006,24(4):549-554.
[3] 王昌勇,郑荣才,田永强,等.陇东地区长9 油层组浅水三角洲沉积特征及成藏条件研究[J].石油天然气学报,2011,33(8):11-15.
[4] 郭艳琴,李文厚,胡友洲,等.陇东地区上三叠统延长组早中期物源分析与沉积体系[J].煤田地质与勘探,2006,34(1):1-4.
[5] 李士春,冯朝荣,殷世江.鄂尔多斯盆地南部中生界延长组沉积体系与油气富集[J].岩性油气藏,2010,22(2):79-83.
[6] 郑荣才,王昌勇,李虹,等.鄂尔多斯盆地白豹—华池地区长6油层组物源区分析[J].岩性油气藏,2007,19(1):32-38.
[7] 王纹婷,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8 油层组物源分析[J].岩性油气藏,2009,21(4):41-46.
[8] 王昌勇,郑荣才,王海红,等.鄂尔多斯盆地姬塬地区长6 油层组物源分析[J].沉积学报,2008,26(6):52-58.
[9] 张绍平,顿铁军.阴极发光显微镜在岩矿鉴定方面的应用[J].西安地质学院学报,1989,11(1):40-49.
[10] 张本琪,余宏忠,姜在兴,等.应用阴极发光技术研究母岩性质及成岩环境[J].石油勘探与开发,2003,30(3):117-120.
[11] 徐惠芬,崔京钢,邱小平.阴极发光技术在岩石学和矿床学中的应用[M].北京:地质出版社,2006:42.
[12] 郑荣才,柳眉清.鄂尔多斯盆地长6 油层组古盐度研究[J].石油与天然气地质,1999,20(1):20-25.
[13] Couch E L. Calculation of paleosalinities fromboron and claymineral data[J]. AAPG Bulletin,1971,55(10):1829-1837.
Outlines

/