There are almost 300×10~4km~2 carbonate rocks distribution area in China, oil and gas pool from the Proterozoic Era to the Cainozoic Era stratum also. It is huge on potential in oil and gas's exploration and exploitation.
我国有近300×10~4km~2的碳酸盐岩分布区,元古代到新生代地层均有碳酸盐岩油气藏,勘探开发潜力巨大。
参考来源 - 川东北裂缝漏失性碳酸盐岩储层损害机理及保护技术研究·2,447,543篇论文数据,部分数据来源于NoteExpress
ADJ → a variant of Cenozoic
The Cainozoic period, was a period of upheaval and extreme volcanic activity.
新生代是一个充满了地壳巨变和剧烈火山活动的时期。
Yingen-Ejina Basins in the west of Nei Mongol is shown by superposition of Mesozoic and Cainozoic on basement of pre-Palaeozoic constitutes.
内蒙西部银根-额济纳盆地群是在 前古生代基底上发育起来的中、新生代“叠 置型”盆地群。
Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the meso - cainozoic detrital rocks in tarim basin.
根据自生矿物与粘土矿物组合,在塔里木中新生界碎屑岩中可以识别出两种成岩环境。
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