地质学
生物地层学
低谷(经济学)
白垩纪
古生物学
经济
宏观经济学
标识
DOI:10.1130/0016-7606(1978)89<151:mpabot>2.0.co;2
摘要
The epeiric sea that flooded the Benue Trough attained a maximum depth of about 30 m during late Turonian time. It encroached from the south and shoaled northeastward with evaporites and carbonates accumulating at the distal end.
科研通智能强力驱动
Strongly Powered by AbleSci AI