盘河断块区馆三段河流相储集层特征及储集性能

2005年 12卷 第01期
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Fluvia l Reservoir Characteristics and Its Reservoir
Property of the ThirdMember of Guantao Formation in
Panhe Fault Block
 王海峰 史洁 侯战胜 刘玉海 郭华 季贤宁 孟令富
 胜利油田有限公司临盘采油厂
L inpan O il Production Plan t,
Shengli O ilf ield Co. L td. , S INOPEC, L iny i 251507,
Ch ina
   盘河断块区馆三段储集层为辫状河流相沉积,从岩性、沉积构造、砂体形态和非均质性质等方面对河流相沉积的性质作了论述。沉积构造有层理、层面构造,砂体形态以箱形及钟形为主。对各小层沉积微相及平面分布进行了研究,主要发育河床滞留沉积和心滩微相。储集性能与沉积微相有较好的对应关系,心滩主体砂体厚度大、物性好、含油饱和度高,其次为心滩边缘,废弃河道较差,储层的含油性还受构造及成岩作用的控制。

The reservoirs of the third member of Guantao formation

in Panhe fault block are mainly braided fluvial sediment, this

article discusses fluvial sedimentary p roperty in lithology,

sedimentary structure, sandbody shape and heterogeneity, its

sedimentary structures are mainly beddings and the structure

of stratified p lane and the shapes of sandbodies are mainly

boxer-like shape and bell shape. so, the author considers that

each formation develop s mainly lag deposit and mid-channel

barmicrofacies according to its sedimentary microfacies and

p lane distributions. Reservoir p roperty and sedimentary

microfacies have better corresponding correlation: the main-

body of mid-channel bars have the p roperty of bigger

thickness, better physical p roperty and higher saturation than

the fringe of mid-channel bar and worse is discussed

riverway, meanwhile, the oil-bearing of reservoir is controlled

by structure and diagenesis.

河流相沉积; 储层特征; 储集性能; 盘河断块区;

Fluvial sediment, Reservoir characteristics,

Reservoir p roperty, Panhe fault block.

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