吉林大学学报(地球科学版)

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基于沉积成岩-储集相分析确定文昌9区低渗储层“甜点”分布

尤丽1,张迎朝1,李才1,张哨楠2,招湛杰1   

  1. 1.中海石油(中国)有限公司湛江分公司, 广东 湛江524057;
    2.西南石油大学地球科学与技术学院, 成都610500
  • 收稿日期:2014-04-09 出版日期:2014-09-26 发布日期:2014-09-26
  • 作者简介:尤丽(1983-),女,工程师,主要从事沉积储层研究,E-mail:rouli456172@sohu.com
  • 基金资助:

    国家科技重大专项(2011ZX05023-001-007);中国海洋石油总公司科研项目(CNOOC-KJ125ZDXM07LTD02ZJ11)

Based on Analysis of Sedimentary-Diagenetic Reservoir Facies to Determine “Sweet Spots” Distribution in Low Permeability from Wenchang 9 Area

You Li1,Zhang Yingzhao1, Li Cai1,Zhang Shaonan2,Zhao Zhanjie1   

  1. 1.China National Offshore Oil Limited CorporationZhanjiang,Zhanjiang524057,Guangdong,China;
    2.School of Geoscience and Technology,Southwest Petroleum University,Chengdu610500,China
  • Received:2014-04-09 Online:2014-09-26 Published:2014-09-26

摘要:

文昌9区位于珠江口盆地文昌A凹陷六号断裂-珠三南断裂带之间。古近系珠海组是主要储集层系,埋深基本大于3 km,为扇三角洲前缘-潮坪相沉积储层,储层物性以低渗特征为主,局部发育中渗。为扩大勘探油气储量和后期合理有效开发,“甜点”储层寻找至关重要,笔者通过常规物性、测井解释、岩石薄片分析、二维核磁共振等,认识成岩相展布与储集层厚度、物性分布,综合沉积作用、成岩作用等,精细剖析珠海组低渗成因及储集厚度与物性差异发育的主控因素。研究表明:珠海组低渗特征形成的主要原因是压实作用,水下分流河道、潮道和砂坪微相为最有利储集相带,其次为混合坪,二者均可能形成“甜点”储层;压实程度偏弱、粒度较粗、溶蚀较强或绿泥石包壳发育区为潜在的“甜点”储层发育区,可确定六号断裂-珠三南断裂带之间发育“甜点”储层;六号断裂带相近埋深,六号断裂带附近区域较远离区域更有利于“甜点”储层发育。

关键词: &ldquo, 甜点&rdquo, 低渗储层, 沉积相, 成岩相, 储集性, 珠海组, 珠江口盆地

Abstract:

Zhuhai Formation is the major reservoir in , Wenchang 9 area between the No.6 Fault and the South Fault of Wenchang A depression,which deeply buried over 3 km. It is the rontal subfacies of fan delta. The reservoir properties are low permeability mainly. In order to expanding the prospecting for oil and gas reserves and later the reasonable and effective development,diagenetic facies and the distribution of reservoir thickness and physical properties are recognized by normal physical characteristics,logging interpretatio,analysis of rock thin and two dimensional nuclear magnetic resonance. The reasons of low permeability formation and factors of reservoir thickness and physics quality are analysed finly from sedimentary facies and diagenesis. It is determined that compaction is the main reseron to low permeability. The most favorable Sedimentary facies are underwater distributary channel,tidal channel,sand flat, the second is the mixed flat. All of them can form “sweet spots” reservoir. Less compaction, coarse grain size, the dissolution stronger intensity or chlorite grain-coatings are the areas of “sweet spots” reservoir. The area between the fault zone 6 to the South fault zone of weaker compaction is “sweet spots” reservoir zone. The zones near the fault are more favorable to sweet spots than the zones further away from the sixth fault with similar depth.

Key words: “sweet spots”, low permeability reservoir, sedimengtary facies, diagenesis facies, reservoir quality, Zhuhai Formation, Pearl River mouth basin

中图分类号: 

  • P618.13
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