Evaluating new fault‐controlled hydrothermal dolomitization models: Insights from the Cambrian Dolomite, Western Canadian Sedimentary Basin

Author:

Koeshidayatullah Ardiansyah1,Corlett Hilary2,Stacey Jack1,Swart Peter K.3,Boyce Adrian4,Robertson Hamish5,Whitaker Fiona5,Hollis Cathy1

Affiliation:

1. School of Natural Sciences University of Manchester Manchester M13 9PL UK

2. MacEwan University Edmonton AB T5J 4S2 Canada

3. Rosenstiel School of Marine and Atmospheric Sciences University of Miami Coral Gables FL 33149 USA

4. Scottish Universities Environmental Research Centre Glasgow G75 0QF UK

5. School of Earth Sciences University of Bristol Bristol BS8 1RJ UK

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference126 articles.

1. Revised models for depositional grand cycles, Cambrian of Western Canada;Aitken J.D.;Bull. Can. Pet. Geol.,1978

2. Birth, growth and death of the Middle Cambrian Cathedral carbonate lithosome, Southern Rocky Mountains;Aitken J.D.;Bull. Can. Pet. Geol.,1989

3. Stratigraphy of the Middle Cambrian platformal succession, Southern Rocky mountains;Aitken J.D.;Geological Survey of Canada Bulletin,1997

4. Multiple fluid flow events and the formation of saddle dolomite: case studies from the Middle Devonian of the Western Canada Sedimentary Basin

5. Impact of basin architecture on diagenesis and dolomitization in a fault-bounded carbonate platform: outcrop analogue of a pre-salt carbonate reservoir, Red Sea rift, NW Saudi Arabia

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