Mobile
Log In Sign Up
Home > english-chinese > "secondary pores" in Chinese

Chinese translation for "secondary pores"

次生孔隙

Related Translations:
breathing pore:  呼吸孔气门,喷水孔
pores filling:  填孔
pore rhomb:  孔菱
pore area:  孔带
pore cluster:  管孔团 多数管孔集合在一起,其数目不定,管孔团常为薄壁细胞所包围孔隙簇微孔团
interlock pore:  通孔
pore zone:  管孔带
pored wood:  有孔材
pore path:  孔道
opening pores:  开鬼门
Example Sentences:
1.2 . reservoir study shows there have been primary and secondary reserving pores developed in the volcanic rock reservoirs of this area , the secondary pore being dominant
储层研究表明,本区火山岩储层主要发育原生和次生两种储集空间,以次生储集空间为主。
2.The diageneses which are destructive to the reservoirs are mainly the filling of minerals in secondary pores , the fissures and the dissolved caverns
对储层起到破坏作用的主要是充填作用,表现为次生溶蚀孔隙、裂缝、溶洞中充填自生矿物,它们的包裹体测温数据证明充填作用发生在埋藏时期。
3.The preserved average porosity is 10 . 1 % at present . the main reservoir space of chang 4 + 52 ~ chang 62 sandstone in the area is secondary pores , especially the secondary intergranular pores
研究区储层砂体的储集空间以次生孔隙为主,并以次生粒间孔隙占优势,次为填隙物内溶孔、粒内溶孔。
4.4 ) the main reservoir of studying region is low pority , low peremeability litharenite and feldspar litharenite with the character of the low component maiturity and middle textural maturity . mostly the reservoir space is secondary pore
研究区储层主要为低孔低渗的岩屑砂岩和长石岩屑砂岩,成分成熟度低,结构成熟度中等。
5.Abstract : yanchang series is a typical low permeability reservoir , and its favourable sandstone reservoir is delta facies . heavy compaction , cementation and heterogeneity exist in it . according to the analysis of the main control factors of forming the secondary pore , it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure . it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism . organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure , and a lot of secondary pore is produced in the runners . from the present exploration result , it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
文摘:陕甘宁盆地三叠系延长统是国内外典型的低渗特低渗油田,储集层主要为三角洲砂体,压实作用和胶结作用强烈,储层非均质性非常严重,因此预测次生孔隙发育带是寻找油气聚集带的关键.通过对陕甘宁盆地陇东地区延长统次生孔隙形成的主控因素分析,认为陕甘宁盆地延长统次生孔隙的形成除了受沉积有利相带控制外,还与地层异常压力的作用密切相关.研究认为陇东地区异常压力的形成机理主要由于成岩过程中粘土矿物脱水作用.粘土矿物大量脱水时间正好与有机质脱羧期相一致,从而在异常压力作用下将生油岩中的大量有机酸及co2带到与之相邻的储集层中,并沿着有利储集相带运移,在酸性水经过的地方形成大量的次生孔隙,为后期油气运聚提供有利通道及宿住空间,从现今的勘探结果来看,通过研究地层异常压力纵横向分布特征,并结合有利相带研究预测次生孔隙育良带是行之有效的方法
6.On the basis of the study of high resolution sequence stratigraphy , this paper discusses the reservoir petrology ' s diagenesis and secondary pore of the chang 4 + 52 ~ chang 62 pay zones in detail by using the methods of analysis of mercury injection , cast section , popular section , scanning electron microscope , x - ray diffraction and etc . the reservoir rock is mainly composed of feldspar fine sandstone , which is characterized by low compositional maturity and relatively high textural mature
本文在高分辨率层序地层学研究的基础上,通过15口井的常规物性、压汞、铸体分析、薄片鉴定、扫描电镜、 x光衍射、阴极发光、粒度分析等多项测试手段,对坪北油田延长组长4 + 52长62储层岩石学、成岩作用及次生孔隙进行了详细研究。
7.Diagenesis not only can change mineral composition , fabric component , and texture , etc . , but more important it can change the reservoir capability greatly , that is , it can build up , or reduce , or enlarge original pores , and even form a series of diagenetic crack . those secondary pores and cracks are important to improve reservoir capability , especially for carbonate
成岩作用不仅使岩石或沉积物的矿物成分结构组分构造等发生程度不同的变化,更重要的是使原岩的储集性能发生很大的变化,即对原生孔隙或堵塞或残留或扩大,而且还可产生一系列的成岩孔缝次生孔缝,这些次生孔缝对岩石储集性的良化,尤其是对碳酸盐岩是至关重要的。
8.The pattern of diagenetic and porosity evolution are established . the primary porosity of the reservoir rocks was 35 % , which was reduced by 21 . 7 % by compaction and pressure solution and 8 . 2 % by cementation . the secondary pores were produced by organic acids " dissolution during organic matter maturing stage , resulting an increase of porosity by 5 %
预测本区砂岩原始孔隙度为35 ,经机械压实和化学压溶作用孔隙度损失了21 . 7 ,后经自生矿物的胶结作用,孔隙度损失了8 . 2 ,当进入有机质成熟阶段,有机酸的溶解作用产生次生孔隙,使孔隙度增加5 ,现今保存的平均孔隙度为10 . 1 。
9.Yanchang series is a typical low permeability reservoir , and its favourable sandstone reservoir is delta facies . heavy compaction , cementation and heterogeneity exist in it . according to the analysis of the main control factors of forming the secondary pore , it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure . it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism . organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure , and a lot of secondary pore is produced in the runners . from the present exploration result , it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure
陕甘宁盆地三叠系延长统是国内外典型的低渗特低渗油田,储集层主要为三角洲砂体,压实作用和胶结作用强烈,储层非均质性非常严重,因此预测次生孔隙发育带是寻找油气聚集带的关键.通过对陕甘宁盆地陇东地区延长统次生孔隙形成的主控因素分析,认为陕甘宁盆地延长统次生孔隙的形成除了受沉积有利相带控制外,还与地层异常压力的作用密切相关.研究认为陇东地区异常压力的形成机理主要由于成岩过程中粘土矿物脱水作用.粘土矿物大量脱水时间正好与有机质脱羧期相一致,从而在异常压力作用下将生油岩中的大量有机酸及co2带到与之相邻的储集层中,并沿着有利储集相带运移,在酸性水经过的地方形成大量的次生孔隙,为后期油气运聚提供有利通道及宿住空间,从现今的勘探结果来看,通过研究地层异常压力纵横向分布特征,并结合有利相带研究预测次生孔隙育良带是行之有效的方法
Similar Words:
"secondary pollution" Chinese translation, "secondary polyploid" Chinese translation, "secondary population" Chinese translation, "secondary pore space" Chinese translation, "secondary pore system" Chinese translation, "secondary porosity" Chinese translation, "secondary porosity index" Chinese translation, "secondary porosity index log" Chinese translation, "secondary porphyria" Chinese translation, "secondary port" Chinese translation