新疆石油地质 ›› 2023, Vol. 44 ›› Issue (4): 404-410.doi: 10.7657/XJPG20230403

• 油气勘探 • 上一篇    下一篇

鄂尔多斯盆地大牛地气田马五5亚段储集层特征及成因

高景云(), 丁晓琪, 祁壮壮(), 田胤瑜   

  1. 成都理工大学 能源学院,成都 610059
  • 收稿日期:2022-08-29 修回日期:2023-01-04 出版日期:2023-08-01 发布日期:2023-08-01
  • 通讯作者: 祁壮壮(1997-),男,河南濮阳人,硕士研究生,油气地质,(Tel)13739497126(E-mail)827996507@qq.com
  • 作者简介:高景云(1998-),男,山东临沂人,硕士研究生,油气地质,(Tel)15552480276(E-mail)1528548555@qq.com
  • 基金资助:
    国家油气重大专项(2017ZX05005)

Characteristics and Genesis of M55 Reservoirs in Daniudi Gas Field, Ordos Basin

GAO Jingyun(), DING Xiaoqi, QI Zhuangzhuang(), TIAN Yinyu   

  1. School of Energy, Chengdu University of Technology, Chengdu, Sichuan 610059, China
  • Received:2022-08-29 Revised:2023-01-04 Online:2023-08-01 Published:2023-08-01

摘要:

鄂尔多斯盆地马家沟组风化壳之下发育一套孔洞型岩溶储集层,是古生界特大型气田的主力储集层,其中,马五5亚段底部见一套裂缝发育的喀斯特扰动相储集层,分布稳定且普遍含气,成因尚不清楚,制约了油气勘探与开发。通过对野外露头和岩心等资料的分析,剖析了该亚段储集层的成因。马五5亚段发育扰动相,发育大量裂缝,野外露头特征明显,成像测井上显示线—斑状模式,裂缝大多被2期方解石充填;扰动相发育在马五5亚段底部,分布于研究区中西部断裂发育区,气测异常明显,勘探前景良好;$马五^{1}_{6}$小层断裂发育,促进了侧向淡水的强烈岩溶作用,形成可容纳空间,上覆地层压力使马五5亚段底部脆性石灰岩形成扰动相储集层。

关键词: 鄂尔多斯盆地, 大牛地气田, 马家沟组, 马五段, 喀斯特, 扰动相, 储集层

Abstract:

A set of vug-type karst reservoirs is developed below the weathering crust of the Majiagou formation in the Daniudi gas field of Ordos basin, which are the main reservoirs of the Paleozoic super-large gas fields. The disturbed-facies karst reservoirs with fractures are found stably at the bottom of the fifth submember of the fifth member of Majiagou formation (M55) and contain gas universally. The genesis of these reservoirs remains unknown, leading to difficulties in oil and gas exploration and development. Based on the analysis on field outcrop and core data, the genesis of the M55 reservoirs was analyzed. Disturbed facies and well-developed fractures are clearly observed from the outcrops, and show a line-porphyritic pattern on the image logging. Most of the fractures are filled by calcite of two periods. The disturbed facies found at the bottom of M55 are mainly distributed in the fault zones of the central and western parts of the study area, with obvious gas logging anomalies and good exploration prospects. Abundant fractures in $\text{M5}^{1}_{6}$ promote the strong karstification of fresh water laterally, forming accommodation spaces. The overburden pressure makes the brittle limestone at the bottom of M55 evolve to disturbed reservoir.

Key words: Ordos basin, Daniudi gas field, Majiagou formation, M5 member, karst, disturbed facies, reservoir

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