The Pennsylvanian epicontinental sea periodically covered much of the Mid-Continent North America during Missourian time, burring the siliciclastic source areas in Kansas-such as the Nemaha uplift and central Kansas ...

The Kopet-Dagh intracontinental basin of northeastern Iran, formed after Middle Triassic orogeny, was

a site of relatively continuous sedimentation from Jurassic through Miocene time. An epicontinental sea

covered ...