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济阳坳陷深层天然气致密砂岩储集空间成因
引用本文:钱峥,赵澄林,刘孟慧.济阳坳陷深层天然气致密砂岩储集空间成因[J].中国石油大学学报(自然科学版),1994(6).
作者姓名:钱峥  赵澄林  刘孟慧
作者单位:石油大学勘探系
摘    要:寻找深层天然气致密砂岩储层中有利的次生孔隙带是深层天然气勘探中值得重视的问题,本文通过分析成岩作用及沉积环境对储集性的影响。对致密砂岩中次生孔隙的成因进行了探讨.认为致密砂岩储集孔间的成因与深层有一定规模的流体运动有关。用流体热对流循环机制较好地解释了深层次生孔隙带的形成,从而指出了济阳坳陷深层天然气的有利分布带。

关 键 词:深层  天然气  储集层  成岩作用  热对流  次生孔隙

GENERATION OFRESERVE SPACES IN DEEPNATURALGAS SANDSTONE RESERVOIRS OF JIYANG DEPRESSION
Qian Zheng, Zhao Chenglin, Liu Menghui.GENERATION OFRESERVE SPACES IN DEEPNATURALGAS SANDSTONE RESERVOIRS OF JIYANG DEPRESSION[J].Journal of China University of Petroleum,1994(6).
Authors:Qian Zheng  Zhao Chenglin  Liu Menghui
Abstract:The key of deep gas exploration is to discover the well-developed porosity zonesin the tight sandstone reservoirs,because the deep natural gas reservoirs are deep in burieddepth,tight in lithological character,senious in diageneses. Examination of more than 180cores from the Eogene sandstones reveals a complex diagenetic history. Diagenetic compexityis a function of depositional environment and burial and thermal history of the depression. The origin of reserve spaces in the tight sandstone is studied.It is considered that the origin ofreserve spaces relates to fluid flow in a great scale in the deep sandstone. The mechanism offluid heat convection cycle cold explains the formation of secondary pore in the deep.So theprediction of deep natural gas detrital reservoir could be defined.
Keywords:Deep zone:Natural gas  Tight sandstone:Reservoir  Secondary pore :Diagenesis  Heat convection:Secondary pore  
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