Deposition is controlled by glacio-eustatic changes, with eolianites forming during interglaciations, and occur along the margins of the global carbonate belt and the carbonate islands along northeastern Yucatan and Rottnest Island.
Deposition is controlled by glacio-eustatic changes, with eolianites forming during interglaciations. Eolianites occur along the margins of the global carbonate belt, on the carbonate islands along northeastern Yucatan, and Rottnest Island.