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苏里格气田下二叠统盒8段异常低压成因及其分布特征
引用本文:陈义才,张胜,魏新善,刘新社,赵惠涛. 苏里格气田下二叠统盒8段异常低压成因及其分布特征[J]. 天然气工业, 2010, 30(11): 30-33. DOI: 10.3787/j.issn.10000976.2010.11.008
作者姓名:陈义才  张胜  魏新善  刘新社  赵惠涛
作者单位:1.成都理工大学;2.四川煤田地质局141队;3.中国石油长庆油田公司勘探开发研究院
摘    要:苏里格气田下二叠统下石盒子组8段(盒8段)异常低压明显,但对其成因未达成共识。为此,统计分析了该区盒8段53口井的实测地层压力,发现产水层、产气层以及气水同产层的地层压力系数在垂向上均无明显变化规律,而在平面上呈南北向的条带状分布,形成多个异常低压系统。应用Fick气体扩散定律和盆地模拟技术,结合区域沉积、构造演化和天然气组成特征分析认为,盒8段河道砂体分布的局限性为异常地层压力的形成提供了必要封闭条件,天然气扩散作用虽然存在,但是扩散损失影响相对较小。盒8段异常低压的形成主要与晚白垩世以来的构造抬升、地层剥蚀以及构造热事件的消失有关。

关 键 词:苏里格气田  早二叠世  异常低压  成因  天然气扩散  盆地模拟  构造运动

Causes and distribution of abnormal low pressure in the 8th member of the Lower Permian Shihezi Formation in the Sulige Gas Field
Chen Yicai , Zhang Sheng , Wei Xinshan , Liu Xinshe , Zhao Huitao. Causes and distribution of abnormal low pressure in the 8th member of the Lower Permian Shihezi Formation in the Sulige Gas Field[J]. Natural Gas Industry, 2010, 30(11): 30-33. DOI: 10.3787/j.issn.10000976.2010.11.008
Authors:Chen Yicai    Zhang Sheng    Wei Xinshan    Liu Xinshe    Zhao Huitao
Affiliation:1.Chengdu University of Technology, Chengdu, Sichuan 610059, China; 2.No.141 Coal Geological Team of Sichuan Coal Geology Bureau, Deyang, Sichuan 618000, China; 3.Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an, Shaanxi 710021, China
Abstract:The 8th member of the Lower Permian Shihezi Formation in the Sulige Gas Field is unusually low in formation pressure. However, the causes of low pressure are not clear. Therefore, the measured formation pressures of this interval in 53 wells are analyzed. The findings indicate that vertically, formation pressure coefficients of water producing layers, gas producing layers and water gas co producing layers show no obvious changing patterns, but laterally, they are in banded distribution, forming several abnormal low pressure systems. Based on an analysis of regional sedimentation, structural evolution and gas components, the Fick gas diffusion law and basin modeling techniques are used to study the causes of abnormal low pressure. It is believed that the limited distribution of channel sands in this interval provides necessary sealing conditions for the abnormal low pressure, and the influences of diffusion loss are relatively small though gas diffusion does exist. The abnormal low pressure in the studied interval is mainly caused by the post Cretaceous structural uplifting, erosion and tectonic thermal events.
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