埃迪卡拉系微生物碳酸盐岩沉积特征及其地质意义:以川中磨溪8井区灯影组四段为例*
罗垚1,2, 谭秀成1,2, 赵东方1,2, 罗文军3, 刘耘3, 肖笛1,2, 乔占峰4, 曾伟1,2

Sedimentary characteristics of the Ediacaran microbial carbonates and their geological implications: a case study of the Member 4 of Dengying Formation from Wellblock MX8 in central Sichuan Basin
Luo Yao1,2, Tan Xiu-Cheng1,2, Zhao Dong-Fang1,2, Luo Wen-Jun3, Liu Yun3, Xiao Di1,2, Qiao Zhan-Feng4, Zeng Wei1,2
川中磨溪8井区埃迪卡拉系灯影组四段叠层石云岩类型 a—平直状叠层石云岩,岩心照片,磨溪21井,5064.45~5064.51 m;b—平直状叠层石云岩,岩心照片,磨溪123井,5478.31 m;c—平直状叠层石云岩,单偏光,磨溪105井,5363.40 m;d—丘状叠层石云岩,岩心照片,磨溪21井,5079.42~5079.51 m;e—丘状叠层石云岩,单偏光,磨溪108井,5300.13 m;f—丘状叠层石云岩,单偏光,磨溪123井,5479.21 m