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1)  southern Shiwu area
十屋南
2)  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% 。
3)  a room with a northern exposure
南屋
4)  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
5)  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。
6)  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 。
补充资料:南中别陈七李十
【诗文】:
二年共游处,一旦各西东。请君聊驻马,看我转征蓬。
画益愁南海,离驹思北风。何时似春雁,双入上林中。



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全唐诗:卷87_45
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