油气地质

麻黄山地区中生界油气分布规律及控制因素分析

  • 董世泰 ,
  • 张立新 ,
  • 徐光成 ,
  • 孙荣
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  • 1.成都理工大学“油气藏地质及开发工程”国家重点实验室; 2.中国石油长庆油田分公司第二采油厂
冯一波,1983 年生,男,成都理工大学在读硕士研究生,从事油气储层评价方面的研究工作。地址:(610059)四川省成都理工大学 能源学院323 室。E-mail:233513124@qq.com

网络出版日期: 2009-09-16

Oil and gas distribution and controlling factors of Mesozoic in Mahuangshan area

  • DONG Shi-tai ,
  • ZHANG Lixin ,
  • XU Guangcheng ,
  • SUN Rong
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  • 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China; 2. NO. 2 Oil Production Plant, Changqing Oilfield Company, PetroChina, Qingyang 745100, China

Online published: 2009-09-16

摘要

鄂尔多斯盆地西缘麻黄山地区中生界具有良好的油气勘探潜力。在对麻黄山地区构造、岩心和测井分析的前提下,探讨了不同构造带的油气分布规律、成藏过程以及油气分布的主要控制因素,认为在构造稳定带主要发育岩性、岩性-构造油气藏,而在断裂带主要发育断块、断鼻油气藏;油气分布纵向上跨度大,为上油下水,具有统一的油水界面,平面上主要分布在构造部位高、砂体发育的背斜或断背斜轴部;油气分布主要受沉积相、成岩作用和构造控制。纵向上胶结作用弱、溶蚀作用强的砂体为油气的主要富集场所,平面上处于构造高部位、水动力强的分流河道与河道砂体为油气的主要富集部位。

本文引用格式

董世泰 , 张立新 , 徐光成 , 孙荣 . 麻黄山地区中生界油气分布规律及控制因素分析[J]. 岩性油气藏, 2009 , 21(3) : 60 -64 . DOI: 10.3969/j.issn.1673-8926.2009.03.012

Abstract

The Mesozoic in Mahuangshan area has a fine hydrocarbon exploration potential in the western margin of Ordos Basin. Based on the analysis of regional structure, core observation and logging, the hydrocarbon distribution, pool forming process and the main controlling factors in different tectonic zones are discussed. It is suspected that lithologic and lithologic-structural reservoirs mainly developed in the structurally stable zones, while fault block and fault-nose reservoirs mainly developed in faulted zones. Oil and gas distribution has a large vertical span with oil on the top and water at the bottom. Oil and gas in the plane mainly distributed in the high structural area or in the axial region of fault anticline, and are mainly controlled by sedimentary facies, diagenesis and tectonic control. The sand of weak cementation and strong dissolution is hydrocarbon-rich site in vertical direction, and so is the sand in distributary channel with strong hydrodynamic in high structural area in the plane.

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