1) Oolitic dolostone
鲕滩云岩
1.
Oolitic dolostone is a vital type of carbonate reservoirs.
鲕滩云岩是重要的碳酸盐岩储层,鲕滩云岩气藏渗透率和含气饱和度的定量计算和预测是气田开发过程中确定储层产能、优选开发层段的基础依据。
2) oolitic dolomite
鲕粒白云岩
1.
High-quality reservoir rocks of oolitic dolomite evolved in 6 sta.
指出古油藏及分散液态烃在燕山中期快速升温条件下,形成高效气源灶,为高效气藏的形成提供了丰富的气源;优质鲕粒白云岩储集层经历6个阶段的演化历史,受控于沉积相带、烃类充注、深埋藏条件下强烈溶蚀以及多期断层活动;二叠系烃源岩与飞仙关组储集层存在强大的剩余压力差,为油气沿断层发生优势输导提供强大动力;燕山晚期—喜马拉雅期的构造作用,使得气藏发生调整与改造。
2.
There are mainly four pore types for oolitic dolomite reservoir in Puguang gasfield,including oolitic dissolution pore,intergranular dissolution pore,dolomite intercrystalline dissolution pore and fractured dissolution pore.
普光气藏鲕粒白云岩储层主要的孔隙类型有鲕粒溶孔、粒间(溶)孔、白云石晶间(溶)孔及裂隙裂缝型(溶)孔。
3) Oolitic shoal
鲕滩
1.
Diagenesis and pore evolution of the oolitic shoal reservoir in the Feixianguan Formation in northeastern Sichuan;
川东北飞仙关组鲕滩储层成岩作用和孔隙演化
2.
The seismic predication of the oolitic shoal reservoirs in Feixian guan Formation, Sichuan basin;
四川盆地铁山坡地区飞仙关组鲕滩储层地震预测
4) oolitic
[,əuəu'litik]
鲕滩
1.
Features of gas accumulation and exploration foreground in oolitic reservoir of Feixianguan Formation in Sichuan Basin;
川东北飞仙关组鲕滩天然气富集成藏特征及勘探前景
2.
It is considered from geologic research that distribution of oolitic and oolitic dolomite is obviously controlled by oceanic trench development.
因此,铁山、双家坝构造也应在飞仙关组具有很好的鲕滩储层。
5) oolite beach
鲕滩
1.
The oolite beach reservoir prediction at Feixianguan formation in Tongnanba structural belt,Northeast Sichuan province
川东北通南巴构造带飞仙关组鲕滩储层预测
2.
The oolite beach of the lower Triassic Feixianguan Formation in eastern Sichuan basin developed in themargin of carbonate platform, and platform margins are always related to ocean trough.
四川盆地东部下三叠统飞仙关组鲕滩主要发育在碳酸盐岩台缘带上,而台缘带与海槽密切相关,找到了海槽就意味着找到了鲕滩。
3.
During the phase of SQ1HST,based on previous deposition,the depth of the basin water gradually turned shallow and the environment changed form the mixing shelf to the open platform;at that time,the oolite beach was developed.
SQ1TST期,由于海平面的上升,研究区发育较深水环境的混积陆棚;进入SQ1HST期由于前期的沉积填充,盆地水体逐渐变浅盆地进入了开阔台地沉积环境,开始了鲕滩发育演化阶段。
6) Oolitic beach
鲕滩
1.
Application of natural gamma inversion in the prediction for the oolitic beach reservoir in Feixianguan Formation in Shuanjiaba Structure;
自然伽马反演在双家坝构造飞仙关组鲕滩储层预测中的应用
2.
Exposition on material base and preservation causes of oolitic beach reservoir in Puguang Gas Field
普光气田鲕滩储层形成的物质基础和保存成因
3.
Changxing Reef of Upper Permian and Feixianguan oolitic beach of Lower Triassic are the focus point of exploration work in Sichuan Basin during the ninth-five-year-plan.
四川盆地上二叠统长兴组生物礁和下三叠统飞仙关组鲕滩是“九五”期间的勘探重点 ,通过对长兴组—飞仙关组气藏的烃源岩、储层沥青和天然气的地球化学研究 ,确认了上二叠统的滨岸煤系泥岩和海槽相碳酸盐岩为主要烃源岩 ,长兴组—飞仙关组气藏天然气主要来源于下伏的上二叠统烃源岩 ,天然气以垂相运移为主 ,飞仙关组部分气藏天然气中硫化氢含量较高与储层中膏岩层的分布和热硫酸盐还原作用有关 ,上述这些特征与沉积相带密切相关。
补充资料：云岩
【云岩】
（人名）潭州云岩寺昙晟，钟陵建昌人，姓王氏，少出家，初参百丈海禅师，侍左右者二十年，未悟玄旨，百丈归寂后，谒药山，言下契会。唐会昌元年，六十而寂。见宋高僧传十一、传灯录十四、五灯会元五。
（人名）潭州云岩寺昙晟，钟陵建昌人，姓王氏，少出家，初参百丈海禅师，侍左右者二十年，未悟玄旨，百丈归寂后，谒药山，言下契会。唐会昌元年，六十而寂。见宋高僧传十一、传灯录十四、五灯会元五。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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