首页 | 本学科首页   官方微博 | 高级检索  
     检索      

川中营山构造须家河组第二段致密砂岩储层特征
引用本文:雍自权,王浩,冯逢,肖尧,翟中华,龚昌明,夏飞勇,徐猛.川中营山构造须家河组第二段致密砂岩储层特征[J].成都理工大学学报(自然科学版),2012,39(2):137-144.
作者姓名:雍自权  王浩  冯逢  肖尧  翟中华  龚昌明  夏飞勇  徐猛
作者单位:1. 油气藏地质及开发工程国家重点实验室(成都理工大学),成都,610059
2. 中国石油西南油气田分公司川中油气矿,四川遂宁,629000
摘    要:四川盆地营山构造须家河组第二段是一套以长石石英砂岩、岩屑长石砂岩为主的地层.通过对须二段储层岩心、薄片观察及物性资料分析,确定须二段属于三角洲前缘亚相,储集砂体由水下分流河道和河口砂坝砂体组成;储集空间类型主要为粒间孔、粒内溶孔;属低孔低渗的裂缝-孔隙型储层.储层发育受沉积、成岩作用双重影响,沉积相是储层形成的基础,成...

关 键 词:营山构造  须家河组  致密砂岩  储层特征

Geological features of tight sandstone reservoir of Member 2 of Xujiahe Formation in Yingshan structure, Central Sichuan, China
YONG Zi-quan , WANG Hao , FENG Feng , XIAO Yao , ZHAI Zhong-hua , GONG Chang-ming , XIA Fei-yong , XU Meng.Geological features of tight sandstone reservoir of Member 2 of Xujiahe Formation in Yingshan structure, Central Sichuan, China[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2012,39(2):137-144.
Authors:YONG Zi-quan  WANG Hao  FENG Feng  XIAO Yao  ZHAI Zhong-hua  GONG Chang-ming  XIA Fei-yong  XU Meng
Institution:1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China; 2.Sichuan Chuanzhong Oil and Gas Mines,CNPC,Suining 629000,China
Abstract:Member 2 of Upper Triassic Xujiahe Formation(T3x2) is a set of debris-feldspar and feldspar-quartz sandstone in the Yingshan structure.Based on the cores,the flake observation and physical properties data of the reservoir in the T3x2,this study indicates that the 2nd member belongs to the front-delta deposition.The main reservoir sandy bodies have deposited in subaqueous distributary channel and distributary mouth bar with intergranular pore and intragranular pores as reservoir space.The reservoir is a cracked-porous type with low porosity and low permeability.The reservoir’s development is influenced by both sedimentary facies and diagenesis.The sedimentary facies is the basis of the development of the reservoir and the diagenesis process controls the reservoir’s ability.Cementation and compaction are the major diagenesis to destroy the pores,and dissolution is the major diagenesis to form the secondary pores.
Keywords:Yingshan structure  Upper Triassic  Xujiahe Formation  tight sandstone  reservoir characteristics
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号