石油与天然气地质 ›› 2013, Vol. 34 ›› Issue (3): 294-300.doi: 10.11743/ogg20130303

• 油气地质 • 上一篇    下一篇

鄂尔多斯盆地延长组长9油层组成藏地质条件

时保宏1, 姚泾利2, 张艳2, 张雷2, 杨亚娟2, 李慧3   

  1. 1. 西安石油大学地球科学与工程学院, 陕西 西安 710065;
    2. 中国石油长庆油田分公司勘探开发研究院, 陕西 西安 710018;
    3. 中国石油长庆油田分公司第七采油厂, 陕西 西安 710018
  • 收稿日期:2012-03-20 修回日期:2013-05-17 出版日期:2013-06-28 发布日期:2013-07-17
  • 作者简介:时保宏(1971- ),男,博士、副教授,油气成藏地质学及天然气地球化学。E-mail:bh.sh@163.com。
  • 基金资助:

    陕西省教育厅项目(11JK0735)。

Geologic conditions for hydrocarbon accumulation in Chang-9 oil reservoir of the Yanchang Formation,Ordos Basin

Shi Baohong1, Yao Jingli2, Zhang Yan2, Zhang Lei2, Yang Yajuan2, Li Hui3   

  1. 1. Xi'an Shiyou University, Xi'an, Shaanxi 710065, China;
    2. Institute of Exploration and Development, PetroChina Changqing Oilfield Company, Xi'an, Shaanxi 710018, China;
    3. The 7th Oil Plant, PetroChina Changqing Oilfield Company, Xi'an, Shaanxi 710018, China
  • Received:2012-03-20 Revised:2013-05-17 Online:2013-06-28 Published:2013-07-17

摘要: 通过对鄂尔多斯盆地长9油层组成藏地质条件的分析,认为长9油藏的油源主要来自于上覆长7油层组和其本身两套烃源岩,但志丹地区长9油藏原油来源于长9烃源岩,无长7烃源岩的混入。长9油层组含油段主要集中在长91亚段,储集体主要发育于辫状河三角洲平原相分流河道砂体及三角洲前缘水下分流河道砂体,部分为半深湖亚相浊积岩砂体。长9储层的岩石类型主要为岩屑长石砂岩,以粒间孔为主,孔隙度、渗透率总体较低。平面上储层物性分布差异性较大,姬塬地区砂岩粒度粗,粒间孔发育,物性最好;而发育碳酸盐胶结物的洛川地区孔隙不发育,物性最差。根据源-储关系,长9油层组主要发育上生下储、自生自储两种成藏组合类型。据综合分析,姬塬地区成藏条件较好,为下一步勘探的最有利区。

关键词: 成藏条件, 长9油层组, 延长组, 鄂尔多斯盆地

Abstract: This paper analyzes the geologic conditions of hydrocarbon accumulation in the Chang-9 reservoir of Ordos Basin.The oil in the Chang-9 reservoir is mixed oil sourced from both the overlying Chang-7 and Chang-9 itself.However,oil in the Chang-9 reservoir in Zhidan area is only sourced from Chang-9 source rocks,without any contribution from the Chang-7 source rocks.The oil mainly occurs in the first segment of Chang-9 oil reservoir.Reservoirs are mainly of distributary channel sandstone of braided river delta plain facies and underwater distributary channel sand of delta front facies,with some turbidites of semi-deep lake facies.Lithology of Chang-9 reservoir is dominated by lithic arkose with well-developed primary inter-granular pores,low porosity and permeability.The physical properties of the Chang-9 oil reservoirs show great lateral variation.In Jiyuan area,the sandstone feature in coarse grain,well-developed inter-granular pores and good poroperm characteristics.In contrast,in Luochuan area,the carbonate cemented sandstone has poor poroperm characteristics due to poor development of pores.According to the relationship between source rocks and reservoirs,two source rock-reservoir combination patterns were identified in Chang-9 oil reservoirs,i.e."upper sourcing" pattern and "indigenously sourcing" pattern.Jiyuan area is the most favorable for further exploration based on comprehensive analysis.

Key words: accumulation condition, Chang-9 oil reservoir, Yanchang Formation, Ordos Basin

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