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
阿曼Qarn Alam地区新元古代微生物岩野外露头相序组合类型及特征(据 Mettraux et al ., 2014 ;有修改) a—向上变浅序,岩性由下至上依次为: 水平纹层岩—波状纹层岩—叠层石—凝块石—纹层岩—蒸发岩—角砾岩;b—由2套向上变浅序列组合而成,岩性由下至上依次为: 叠层石—凝块石—波状纹层岩—叠层石—凝块石—波状纹层石