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Welcome to the new Datapages Archives

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The AAPG/Datapages Combined Publications Database

Showing 20,863 Results. Searched 200,639 documents.

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Abstract: Sedimentology of Composite Sand-and-Gravel Beach-Shoreface Complexes; #90171 (2013)

Shannon E. Frey and Shahin E. Dashtgard

Search and Discovery.com

... water depth. Strong tidal currents dominating over weak wave processes in the lower shoreface could result in coarser-grained sediments being deposited...

2013

Are Tides Controlled by Latitude?

Search and Discovery.com

N/A

ABSTRACT: Sequence Stratigraphy in a Black Shale Succession: Recognition of Rising and Falling Sea Level in the Chattanooga Shale; #90007 (2002)

Juergen Schieber

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... starved basin succession, deposited far from shore in comparatively deep water. Recognition of evidence for wave reworking and laterally persistent...

2002

ABSTRACT: A Comparison of Late Quaternary Deltaic/Estuarine Depositional Systems from Wave- and Tide-Dominated Shelves; #90007 (2002)

Serge Berne, Gilles Lericolais, Pierre Vagner, Marina Rabineau

Search and Discovery.com

...ABSTRACT: A Comparison of Late Quaternary Deltaic/Estuarine Depositional Systems from Wave- and Tide-Dominated Shelves; #90007 (2002) Serge Berne...

2002

ABSTRACT Sediment Dispersal Across Late Cretaceous Shelf Western Interior Seaway Northern Utah and Colorado USA, #90104 (2010)

Hampson Gary

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... was dispersed via wave‐dominated deltaic systems with a “compound clinoform”  geomorphology in which an inner, wave‐dominated shoreface clinofom...

2010

ABSTRACT Decoupling of the Sevier Foreland Basin from the Cretaceous Western Interior Seaway During Lowstand Events, #90104 (2010)

Kamola Diane L.; Hoffmeister Kathryn E.

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... indistinguishable from the main portion of the KWIS.  This is especially significant during highstand events when shorelines were wave dominated and prograded...

2010

ABSTRACT Shelf Physiography and Accommodation as Controls on Permian Grainstone Bodies, #90104 (2010)

Kerans Charlie; Harris Paul M.

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..., with their steeper, higher‐relief/energy  margins, contain both wave‐ and tide‐dominated sand‐bodies with dip dimension (0.5‐5 km), bedform size up to 2 m...

2010

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