西南石油大学学报(自然科学版) ›› 2010, Vol. 32 ›› Issue (2): 7-12.DOI: 10.3863/j.issn.1674-5086.2010.02.002

• 地质勘探 • 上一篇    下一篇

新沟咀组下段粘土矿物分布特征与储层敏感性

陈恭洋 张玲 周超宇   

  1. 长江大学计算机科学学院,湖北 荆州 434023
  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:2010-04-20 发布日期:2010-04-20

THE DISTRIBUTION CHARACTERISTICS OF CLAY MINERALS AND RESERVOIR SENSITIVITY IN THE LOWER SECTION OF XINGOUJU FORMATION

CHEN Gong-yang ZHANG Ling ZHOU Chao-yu   

  1. College of Computer Science,Yangtze University,Jingzhou Hubei 434023,China
  • Received:1900-01-01 Revised:1900-01-01 Online:2010-04-20 Published:2010-04-20

摘要:

江陵凹陷新沟咀组下段粘土矿物组合与分布受沉积环境影响明显,高岭石仅分布于三角洲平原相带中,粘土矿物以伊利石、高岭石和有序-无序伊蒙混层及少数绿泥石为特征;三角洲前缘相中粘土矿物组合则为伊利石、绿泥石和有序伊蒙混层;前三角洲及湖盆泥岩相中则以伊利石和绿泥石两种粘土矿物为主。储层的敏感性实验结果表明,本区储层具有中等强度速敏、强—特强水敏、强盐敏和强酸敏性。

关键词: 江陵凹陷, 新沟咀组, 粘土矿物, 敏感性实验, 储层损害

Abstract:

The combination and distribution of clay minerals in lower section of Xingouju Formation of Jiangling sag are obviously controlled by the sedimentary environment,kaolinite exists only in delta plain facies,the minerals are characterized by illite,kaolinite,ordered to disordered illite/montmorillonite mixing layer and small amount of chlorite.The clay minerals combination in delta front facies include illite,chlorite and ordered illite/montmorillonite mixing layer.The two main clay minerals in prodelta and lacustrine mudstone are illite and chlorite.The sensitivity test result shows that the reservoir has medium velocity sensitivity,strong-superstrong water sensitivity,strong salt sensitivity and strong acid sensitivity in the study area.

Key words: Jiangling sag, Xingouju formation, clay minerals, sensitivity test, reservoir damage

中图分类号: