中国石油勘探 ›› 2020, Vol. 25 ›› Issue (3): 146-155.DOI: 10.3969/j.issn.1672-7703.2020.03.013

• 石油地质 • 上一篇    下一篇

鄂尔多斯盆地东南部奥陶系岩溶古地貌与储层分布规律

曹红霞1,2 ,吴海燕2 ,任星民2 ,武渝2 ,梁全胜2 ,仝敏波3   

  1. 1 大理大学;2 陕西延长石油(集团)有限责任公司研究院;3 陕西煤业化工技术研究院有限责任公司
  • 出版日期:2020-05-15 发布日期:2020-05-15
  • 基金资助:
    国家自然科学基金资助项目“鄂尔多斯盆地南缘三叠系延长组优质烃源岩中碳酸岩的发现及其成因研究”(41702117); 陕西省自然科学基金资助项目“基于分形理论的致密碳酸盐岩储层微纳米孔喉结构定量表征研究”(2017JQ4007);陕西省自然科学基础 研究计划资助项目“渭河盆地油气地质条件及勘探潜力研究”(2017JQ4018)。

Karst paleogeomorphology and reservoir distribution pattern of Ordovician in the southeastern Ordos Basin

Cao Hongxia1,2, Wu Haiyan2, Ren Xingmin2, Wu Yu2, Liang Quansheng2, Tong Minbo3,   

  1. 1 Dali University; 2 Research Institute of Shaanxi Yanchang Petroleum (Group) Co.,Ltd.; 3 Shaanxi Coal and Chemical Technology Institute Co.,Ltd
  • Online:2020-05-15 Published:2020-05-15
  • Supported by:
     

摘要: 为研究鄂尔多斯盆地东南部岩溶古地貌发育特征及储集空间分布规律,依据岩心、测井、露头、地震、 分析化验等资料,采用古地质图法、残余厚度法、印模法、地球物理属性法等方法进行综合分析,得出鄂尔多斯盆地 东南部奥陶系岩溶古地貌形态为:“西与西南为高地,高中可见鞍与台,台间洼地汇流水,水流沿坡向东流,坡中形 成丘与台,丘台间有若干沟,沟沟相汇进入盆,盆中可见洼与丘”。研究认为,岩溶斜坡中残丘、岩溶高地与岩溶台 地转换部位、古沟槽两侧上倾方向的斜坡带岩溶作用强烈,溶蚀孔隙发育。由于受后期压实、胶结、交代、溶蚀等成 岩作用影响,原生孔隙保留很少,储层储集空间以纳米级晶间孔为主,其次为微米级的溶蚀孔。根据岩溶古地貌与古 沟槽网络分布规律及储层储集空间分布特征,认为古沟槽控制的斜坡带及残丘区、岩溶高地的地貌单元转换带是勘探 开发的重点区域。

 

关键词: 碳酸盐岩, 岩溶古地貌, 储层研究, 马家沟组, 鄂尔多斯盆地东南部

Abstract: In order to study the development characteristics of karst paleogeomorphology and the spatial distribution pattern of reservoir in the southeastern Ordos Basin, based on data from cores, well logging, outcrop, seismic data, and laboratory testing, several methods, such as paleo-geological mapping, residual thickness, and impression and geophysical attributes, are used for comprehensive analysis. Results show that the karst paleogeomorphology of the Ordovician in the southeastern Ordos Basin is as follows: “The west and the southwest areas are highlands, where saddles and platforms are developed. Water funnels into sags between platforms and flows eastward along the slope. Mounds and platforms are formed in the slope, between which there are several grooves. Water in the grooves finally funnels into the basin. There are sags and mounds in the basin.” The study shows that, in residual mounds, karst highlands, and transitional parts of karst platforms in karst slopes, as well as in the slope zones of the up-dip parts of paleo grooves, karstification is strong and dissolution pores are well developed. Due to the influence of later diagenesis such as compaction, cementation, metasomatism and dissolution, primary pores are rarely preserved. The reservoir space is mainly composed of nanometer-scale intercrystalline pores, followed by micro-scale dissolution pores. According to the distribution patterns of karst paleogeomorphology and paleo groove networks, and the spatial distribution characteristics of reservoir space, the slope zones and residual mound areas controlled by paleo grooves and the geomorphic transition belts in karst highlands are the key areas for hydrocarbon exploration and development.

Key words: carbonate rock, karst paleogeomorphology, reservoir study, Majiagou Formation, southeastern Ordos Basin

中图分类号: