摘要
根据塔北地区钻井实测地层压力、声波时差与深度的关系以及地震剖面处理所计算的地层压力等资料，分析了塔北地区地层压力的纵、横向分布特征后指出，在剖面上存在着苏维依（Ｎｓ）—志留系，寒武系下部—震旦系两个异常高压带；阿克库勒地区石炭系见有明显的压力异常，可构成压力封闭层，这对于下伏层系晚期油气藏的保存十分有利。
On the basis of measured formation pressure by drilling, the relation of interval transit time and depth as well as formation pressure calculated from seismic profile, this paper analyzed distribution characteristics of formation pressure in vertical and lateral directions, suggested that there are two abnormal high pressure belts in seismic profile including Suweiyi formatiom-Silurian and Lower Cambrian-Sinian, and obvious pressure anomaly occurred in Carboniferous in Akekule area, which could form confining pressure zone, being very favourable for preservation of latestageformed reservoirs under underlying strata.
出处
《新疆石油地质》
CAS
CSCD
1998年第2期121-125,共5页
Xinjiang Petroleum Geology
基金
"八五"国家科技攻关85-101项目
关键词
塔里木盆地
地层压力
油气藏
封闭压力
分布特征
Tarim basin Formation pressure Distribution Reservoir Abnormal pressure Confining pressure
