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柴达木盆地红柳泉构造下干柴沟组下段岩性油藏主控因素

牟中海1 马力宁2 马达德2 廖 锐1 徐良威1   

  1. 1 西南石油大学地球科学与技术学院;2 中国石油青海油田公司
  • 出版日期:2014-12-15 发布日期:2014-12-15
  • 作者简介:牟中海(1960-),男,陕西宝鸡人,博士,2005 年毕业于西南石油大学,教授,现主要从事石油地质学与油藏描述方面 的研究工作。地址:四川省成都市新都区新都大道8 号,邮政编码:610500。E-mail:SWPUMZH@163.com
  • 基金资助:
    中国石油天然气股份有限公司重大科技专项柴达木盆地老区稳产提高采收率技术研究成果(2011E-0306)。

Main Controlling Factors of Lithologic Reservoirs of Lower Ganchaigou Formation below Hongliuquan Structure of Qaidam Basin

Mou Zhonghai1, Ma Lining2, Ma Dade2, Liao Rui1, Xu liangwei1   

  1. 1 School of Geoscience &Technology, Southwest University of Petroleum; 2 PetroChina Qinghai Oilfi eld Company
  • Online:2014-12-15 Published:2014-12-15

摘要: 通过地质、地震、测井、分析化验资料的综合分析,从沉积作用、成岩作用、断裂作用3 个方面,对柴 达木盆地红柳泉构造下干柴沟组下段(E3 1)岩性油藏成藏的三大控制因素——沉积微相、胶结作用、微断层进行了分析。 研究认为红柳泉构造下干柴沟组下段岩性油藏并非相控,沉积微相只控制砂体的分布。压实作用主要使储层变得致密, 储集性能变差,但对物性或含油气性在横向上的变化影响不大;胶结作用在红柳泉构造上倾方向产生封堵,大致在红 113 井、红22 井、红15 井一线形成封堵带,并使油气主要聚集于斜坡带中部,胶结矿物主要是硬石膏、石膏、方解 石等。微断层发育区是红柳泉构造油气主要分布区,不同微断层封堵条件的差异则是岩性油藏的重要控制因素,造成 了相邻井含油气性的明显差异。

关键词: 中扬子地区, 海相, 天然气, 台缘礁滩, 岩溶, 勘探方向, 勘探对策

Abstract: Based on comprehensive analysis of geological, seismic, logging and testing data and focusing on three areas of sedimentation, diagenesis and breaking effect, this paper elaborates three main controlling factors of lower lithologic reservoirs of lower Ganchaigou Formation (E31) below Hongliuquan Structure of Qaidam Basin – sedimentary microfacies, cementation and micro faults. The study indicates that the lithologic reservoirs of the E31 in Hongliuquan Structure is not facies controlled and the sedimentary microfacies only controls distribution of sand bodies. Compactness makes the reservoir compact but exerts little impact on horizontal changes in physical properties and oil bearing properties of the reservoirs. Cementation results in sealing in the updip direction of Hongliuquan Structure, leading to a sealing zone along Hong 113 Well, Hong 22 Well and Hong 15 Well. Therefore, oil and gas are accumulated mainly in the middle position of the slope zone. Cementation minerals are mainly anhydrite, gypsum and calcite. Micro fault development zone is the main oil and gas bearing zone in Hongliuquan Structure. The differences in sealing conditions of different micro faults are the important controlling factors for lithologic reservoirs, causing the apparent difference in the oil bearing properties of neighboring wells.