孔隙特征 meaning in Chinese
pore character
Examples
- Bituminous mixtures - test methods for hot mix asphalt - part 8 : determination of void characteristics of bituminous specimens
沥清混合物.热拌沥清混合料试验.第8部分:沥青样件孔隙特征的测定 - Abstract : the petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method , the quantitative mineral clay analysis method and thin - section analysis method . based on the study , the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance . the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed
文摘:利用x衍射全岩分析方法、粘土矿物定量分析方法和薄片鉴定等方法研究了城华地区延8 -延10储层岩石学特征和孔隙成因类型.综合论述了城华地区延8延10油组不同岩相储层砂岩的基本特征，纠正了砂岩定名的错误和主要填隙物成份的错误，同时还论述了储层砂岩的孔隙特征和控制孔隙发育的主要因素 - The petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method , the quantitative mineral clay analysis method and thin - section analysis method . based on the study , the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance . the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed
利用x衍射全岩分析方法、粘土矿物定量分析方法和薄片鉴定等方法研究了城华地区延8 -延10储层岩石学特征和孔隙成因类型.综合论述了城华地区延8延10油组不同岩相储层砂岩的基本特征，纠正了砂岩定名的错误和主要填隙物成份的错误，同时还论述了储层砂岩的孔隙特征和控制孔隙发育的主要因素 - In this paper , thermal evolution history of organic matter of the source rocks and hydrocarbon generation history have been researched by tti method , hydrocarbon migration direction and migration times were probed combining with the area structure development feature ; distribution pattern of the main reservoir intervals on lateral and longitudinal have been predicted by researching on development feature and control factors of the reservoir intervals , the actions of reservoir conditions in hydrocarbon accumulation and bearing also were probed combining with pore evolution feature ; the micro - pore feature of regional cap and direct seal in carboniferous - lower triassic in this area have been determined with micro - capillary pressure curve and intrusive mercury curve ; the prospecting districts have been pointed out combining with the hydro - geologic feature , the potential reservoirs were classified according to trap types in this area , the author attempt to evaluate on the hydrocarbon - bearing condition in the str ata of carboniferous ~ lower triassic from hydrocarbon generation and migration reservoir condition , reserved condition etc , and predict the reservoir types and hydrocarbon - bearing patterns combining with the structure evolution . based on above , the author point out that the central block of chenghu - tuditang synclinorium and the southern block of dangyang synclinorium are the advantageous regions for exploration
本文用tti方法研究了烃源岩有机质的热演化史和油气生成史，并结合区内构造发育特征，探讨油气在区域上的运移方向和在时间上的运移期次；通过对储集层段的发育特征和控制因素的研究，预测了本区主要的储集层段在横向上和纵向上的分布规律，并结合孔隙演化特征，探讨储集条件在油气聚集成藏中的作用；利用微毛细管压力曲线法和压汞法，对石炭系?下三叠统的区域盖层和直接盖层的微孔隙特征进行了定量评价，并结合水文地质分布特征，指出有利于油气保存的地区；根据区内存在的各种圈闭类型，对可能存在的油气藏进行了分类，并试图从油气的生成与运移、储集条件、保存条件等方面，动态地综合评价石炭系?下三叠统油气成藏条件，并结合构造演化特征，预测其油气藏类型和成藏模式。