1) Feixianguang Ertan formation
飞仙关鲕滩
3) oolitic shoal of the third section of Feixianguan Formation
飞三鲕滩
4) 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
5) 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。
6) 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。
补充资料：飞沙关
飞沙关在汶川县映秀镇上约34公里处，因山势陡险，飞沙射人，昔有关卡，故名。民间盛传，贵妃杨玉环幼年曾于该处洗浴，时有羌男在河岸偷觑，贵妃察觉后取沙投射，从此该地飞沙射人，得名飞沙关。 该关是刳儿坪向下延伸的山脊，直抵岷江江心，悬崖近百米，岷江鼓浪击崖，轰然飞沫，跌落成漩。 1952年前，这里悬崖绝壁，山路仅能通一马。关上有一券门，门上有一长方形石匾，上刻“飞沙关”三大字，今已经毁。今崖上有圣母祠，已废，侧壁有诗刻，为清人孟维聪所作。1953年在崖中凿一洞，成阿公路穿洞而去，为该路唯一隧道洞。飞沙关四周灌木零星，蒿草遍野，川西王百合，开于初夏。
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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