1) southern part of Shiwu depression
十屋断陷南部
1.
Because of compaction and cementation by carbonate, silicon and argillan, the pore loss of lower cretacious reservoir bed of southern part of Shiwu depression is 25%~30%.
十屋断陷南部下白垩统储层因压实作用和碳酸盐、硅质、粘土膜胶结作用损失的孔隙度达 25%~30% 。
2) Shiwu fault depression
十屋断陷
1.
Study on the period and time of oil and gas accumulation in the Shiwu fault depression of the southern Songliao Basin,China;
松辽盆地南部十屋断陷成藏期次研究
2.
Oil-gas accumulation rules of Shiwu fault depression at southeast uplift area of Songliao basin.;
松辽盆地东南隆起区十屋断陷油气聚集规律
3.
Diagenesis of the Shiwu fault depression in southern part of Songliao basin;
松辽盆地南部十屋断陷成岩作用
3) Shiwu faulted depression
十屋断陷
1.
Characteristics of surface hydrocarbon anomalies in Shiwu faulted depression in southern Songliao basin and their significance as an oil/gas indicator;
松辽盆地南部十屋断陷地表烃类异常特征及油气指示意义
2.
Shiwu Faulted depression experienced two stages of evolution which are early fault depression and late vanish.
十屋断陷经历了早期断陷和晚期消亡两大发育阶段 ,依据不整合面及对应的整合面 ,可划分出 2个超层序、4个层序 ,分别与构造演化阶段相匹配。
3.
Therer are two kinds of geochemical anomaly zones in Shiwu faulted depression.
松辽盆地十屋断陷存在两类地表化探异常带 :一类为油气沿嫩末运动形成或复活的断裂运移至地表所致 ,具有物上气仍然活跃的特点 ;另一类为油气通过微渗漏所形成 ,具有ΔC、酸解烃及物上气高异常的特点。
4) Shiwu depression
十屋断陷
1.
Water-rock interaction in the Shiwu Depression, Songliao Basin, NE China;
松辽盆地十屋断陷流体-岩石相互作用
2.
Underpressure system developed in the Shiwu depression of Songliao basin with measured formation pressure gradient ranging between 0.
松辽盆地东南隆起区十屋断陷发育异常低压体系 ,实测的地层压力梯度介于 0 。
5) Shiwu rift
十屋断陷
1.
The deposition system analysis of Shiwu rifted stratum in the south of Songliao basin;
松辽盆地南部十屋断陷层沉积体系类型及特征
2.
After studying the data of the central structural belt in Shiwu rift ,southern Songliao basin, it is found that there are several structural-lithologic composite traps ,such as the structure to the west of SN85 well, the structure to the northern SN87 well and No.
松南十屋断陷中央构造带实际资料研究 ,发现了几个构造 -岩性复合圈闭 ,即SN85井西构造、SN87井北构造、孤家子北构造。
6) Shiwu faultdown
十屋断陷
1.
The kinds, density and open width of the fractures in Shiwu faultdown are studied systematically, in which the mechanics and factors controlling fractures are mentioned.
以松辽盆地东南缘十屋断陷为例,详细研究了储集层内分布的裂隙类型、密度、张开度。
补充资料:断陷盆地
断陷盆地
指断块构造中的沉降地块,又称地堑盆地。它的外形受断层线控制,多呈狭长条状。盆地的边缘由断层崖组成,坡度陡峻,边线一般为断层线。随着时间的推移,在断陷盆地中充填着从山地剥蚀下来的沉积物,其上或者积水形成湖泊(如贝加尔湖、滇池),或者因河流的堆积作用而被河流的冲积物所填充,形成被群山环绕的冲积、湖积、洪积平原。如太行山中的山间盆地和地堑谷中发育着的冲积洪积平原。低于海平面的断陷盆地被称为大陆洼地。
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