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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 98-104

Tide-influenced Channel Deposits in the Lower Cretaceous Glauconitic Member, Southern Alberta

G. E. Reinson

Abstract

In the subsurface of southern Alberta, the Glauconitic sandstone member of the lower Cretaceous Mannville Group contains channel-fill sandstone deposits interpreted to have formed in an estuarine environment under the influence of tides. The channel sandstones display physical sedimentary structures (bundles, mud-layer couplets) which are characteristic of Holocene estuarine tidal deposits. The channel sandstones are in gradational relationship with bioturbated interstratified sandstone-mudstone lithofacies which are thought to represent lateral accretion bedding associated with subtidal estuarine channel point-bar deposits.


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