Build-ups and hydrocarbon accumulation of the isolated carbonate platforms in the eastern Mediterranean |
WEN Zhixin,TONG Xiaoguang,GAO Huahua,WANG Zhaoming,CHEN Ruiyin,SONG Chengpeng,HE Zhengjun,LIU Zuodong,KANG Hailiang |
Fig. 6. Microscopic and macroscopic petrological characteristics of ESM isolated platform (according to reference [14]). (a) Well ODP967, 370 m, Upper Cretaceous Cenomanian, organic-rich foraminiferous marl, with lighter irregular biological burrows, plane polarized light; (b) Well ODP966, Eocene, laminar organic-rich black micrite limestone, with biological burrows and small horizontal strain shadow; (c) Well ODP966, 163 m, Miocene, coral bioclast, plane polarized light; (d) Well ODP965, 77 m, Miocene, grainstone, with intercrystalline pores and molded pores. |