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The AAPG/Datapages Combined Publications Database

CSPG Special Publications

Abstract


Modern and Ancient Examples of Clastic Tidal Deposits: A Core and Peel Workshop, 1989
Pages 37-49

Estuarine Channel Fills in the Upper Cretaceous Dunvegan Formation: Core Examples

Janok Bhattacharya

Abstract

The Upper Cretaceous Dunvegan Formation of western Alberta has been subdivided into seven allomembers (A to G), each separated by widespread transgressive flooding surfaces.

Wave-dominated, deltaic, depositional systems in member D are fed by a major distributary channel in the Waskahigan area. Channel fill facies comprise basal sandstones exhibiting tidal cross-bedding overlain by thick, brackish marine mudstones. The channel is interpreted to have been filled as a microtidal estuary during the initial phase of transgression of member D.


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