Dana Ulmer-Scholle - Academia.edu (original) (raw)

Papers by Dana Ulmer-Scholle

Rapport Grønlands Geologiske Undersøgelse

The depositional pattern of the Upper Permian Wegener Halvø Formation is mainly controlled by the... more The depositional pattern of the Upper Permian Wegener Halvø Formation is mainly controlled by the karst topography of the surface of the underlying Karstryggen Formation. The area was divided by a NNW–SSE trending depositional and/or erosional high during Late Permian times. Peritidal carbonates and evaporites are dominant on the platform to the west while to the east oolite and biogene grainstone deposits dominate. Reservoir-quality properties are mainly confined to the grainstone deposits east of the high.

Rio Grande rift: Northern New Mexico

Guidebook 67 - Geology of the Belen Area

A Color Guide to the Petrography of Sandstones, Siltstones, Shales and Associated Rocks

Rapport Grønlands Geologiske Undersøgelse

The depositional pattern of the Upper Permian Wegener Halvø Formation is mainly controlled by the... more The depositional pattern of the Upper Permian Wegener Halvø Formation is mainly controlled by the karst topography of the surface of the underlying Karstryggen Formation. The area was divided by a NNW–SSE trending depositional and/or erosional high during Late Permian times. Peritidal carbonates and evaporites are dominant on the platform to the west while to the east oolite and biogene grainstone deposits dominate. Reservoir-quality properties are mainly confined to the grainstone deposits east of the high.

Rio Grande rift: Northern New Mexico

Guidebook 67 - Geology of the Belen Area

A Color Guide to the Petrography of Sandstones, Siltstones, Shales and Associated Rocks