Skip to Main Content
Skip Nav Destination

A carbonate buildup was cored in the Lower Cretaceous Shuaiba Formation of the eastern Arabian Peninsula. The sequence is 58 m (190 ft) thick and consists of a basal algal bank overlain by a bioherm composed of caprinid rudists with point-to-point contact in a muddy matrix. Upward growth of the bioherm into the surf zone led to development of extensive sheets of skeletal sand and gravel. Subsequent subaerial exposure and fresh water leaching led to creation of secondary moldic and microvugular porosity.

Proximity to open basins, a pre-existing topographic high, and either rapid subsidence or eustatic rise to channel...

You do not currently have access to this chapter.

Figures & Tables





Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal