飞仙关组原称“飞仙关页岩”，属于早三叠世早期地层。最初命名地点在中国四川广元市飞仙关，故名。
三叠系飞仙关组 feixianguan formation of triassic
The research shows that the development of gas reservoir of the Feixianguan formation in northern Sichuan Basin mainly controlled by the Kaijiang-Liangping inter-platform basin, and distributed around the Kaijiang - Liangping inter-platform basin.
多年的研究表明，川东北飞仙关组气藏主要环开江-梁平台盆发育，受台盆分布范围的控制。
参考来源 - 渝东—鄂西地区早中三叠世层序岩相古地理研究·2,447,543篇论文数据，部分数据来源于NoteExpress
川东地区飞仙关组储层的发育，受有利沉积相带控制。
Development of reservoir in Feixianguan formation of east Sichuan is controlled by favorable sedimentary facies.
应用测井资料识别川东飞仙关组鲕滩储层是个新课题。
It is a new problem to identify the oolitic beach reservoirs of Feixianguan Formation in East Sichuan by log data.
研究表明，飞仙关组储层主要受沉积作用和成岩作用的控制。
Study suggests that Feixianguan formation is essentially controlled by sedimentation and diagenesis.
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