Models for Carbonate Stratigraphy from Miocene Reef Complexes of Mediterranean Regions
Models for Carbonate Stratigraphy from Miocene Reef Complexes of Mediterranean Regions
复制标题
地中海地区中新世珊瑚礁复合体的碳酸盐地层模型
DOI：
10.2110/csp.96.05
复制
发表时间：
1996
影响因子：
2.5
通讯作者：
J. Rouchy
中科院分区：
文献类型：
--
作者：
E. Franseen;M. Esteban;W. Ward;J. Rouchy
中新世碳酸盐在地中海地区的部分地区进行了密集勘探，并在当地开采碳氢化合物。本出版物中提出的露头模型为伊朗、伊拉克和苏伊士湾的高产中新世碳酸盐岩以及其他地区的小型储层提供了很好的类比。地中海地区露头的经验教训同样适用于中新世碳酸盐岩储层。地中海地区中新世露头可以作为碳酸盐岩储层、蒸发前盆地沉积物和上覆蒸发岩之间关系的模型。此外，在地中海地区暴露的中新世碳酸盐岩可以作为古碳酸盐岩边缘盆地有或没有盆地蒸发岩的重要类比物。
Miocene carbonates are intensively explored and locally exploited for hydrocarbons in parts of the Mediterranean regions. The outcrop models presented in this publication provide excellent analogs for the highly productive Miocene carbonates from Iran, Iraq and Gulf of Suez and for smaller reservoirs in other localities. Lessons learned in the outcrops of the Mediterranean regions are applicable as well to Miocene carbonate reservoirs. The Miocene outcrops in Mediterranean regions can serve as models for the relationships between carbonate reservoirs, pre-evaporitic basinal sediments, and overlying evaporites. Additionally, the Miocene carbonate rocks exposed in the Mediterranean regions serve as important analogs for ancient carbonate-rimmed basins with or without basinal evaporites.