四川盆地二叠系龙潭组页岩孔隙发育特征及主控因素
陈斐然(
),魏祥峰,刘珠江,敖明冲,燕继红
),魏祥峰,刘珠江,敖明冲,燕继红
Pore development characteristics and main controlling factors of the Permian marine-continent transitional shale in the Sichuan Basin
Fei-ran CHEN(),Xiang-feng WEI,Zhu-jiang LIU,Ming-chong AO,Ji-hong YAN
),Xiang-feng WEI,Zhu-jiang LIU,Ming-chong AO,Ji-hong YAN
图12. DYS1井龙潭组黏土矿物含量[（a)—(c）]利川沙溪吴家坪组硅质矿物含量[（d)—(f）]与孔容及TOC相关性
Fig. 12. Correlation between the clay mineral content [（a)-(c）] of Longtan Formation in Well DYS1 and the siliceous mineral content [（d)-(f）] of Wujiaping Formation in Lichuan with pore volume and TOC
