四川盆地龙岗气田三叠系飞仙关组储集层特征及成因机理*
祝海华1,2, 钟大康1,2

Characteristics and formation mechanism of the Triassic Feixianguan Formation reservoir in Longgang Gas Field,Sichuan Basin
Zhu Haihua1,2, Zhong Dakang1,2
龙岗气田三叠系飞仙关组碳酸盐岩储集层岩石类型 a—泥晶鲕粒灰岩,粒间孔被泥晶方解石全部胶结,孔隙不发育,单偏光,龙岗17井,5823.0 m;b—细晶砂屑灰岩,单偏光,龙岗39井,6409.0 m;c—亮晶白云化(质)鲕粒灰岩,单偏光,龙岗19井,5688.5 m;d—鲕粒白云岩,溶蚀孔隙发育,单偏光,龙岗21井,5649.0 m;e—铸模孔白云岩,单偏光,龙岗21井,5644.5 m;f—细晶白云岩,白云石晶间孔极发育,有溶蚀扩大特征,单偏光,龙岗28井,5763.0 m