摘要
研究了南海北部大陆边缘盆地活动热流体的基本物理参数——异常地层压力,探讨了地层压力的预测方法,分析了声波时差与实测地层压力的矛盾,并采用了综合参数预测的有效方法,从理论上建立正常压实趋势线的数学模型;运用该模型计算了异常压力的下界面和建立了压力囊的断面图;计算并分析了高压顶面压力系数。
The abnormal high geopressure, one of the basic physical parameters of the active heat fluid in the continental marginal basin, north of the South China Sea, have been studied. The effective prediction methods were used after analyzing the contradiction of the sonic transit time and the observed geopressure. The mathematical model of normal compaction trend has been established in theory, which was used to calculate the geopressure coefficient and the sub-surface of the high geopressure and build the cross section of the geopressure chambers. The places favourable for the hydrocarbon accumulation were pointed out by analyzing the geopressure coefficient, gas potential and water potential.
出处
《地球科学(中国地质大学学报)》
CSCD
北大核心
1996年第1期84-88,共5页
Earth Science-Journal of China University of Geosciences
基金
国家自然科学基金
关键词
地层压力
热流体
预测法
南海
地下热流
continental marginal basin
abnormal geopressure
active heat fluid
prediction method.