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GEOREF RECORD
The solution brecciation process
Robert J. Stanton
The solution brecciation process
Geological Society of America Bulletin (1966) 77 (8): 843-847
The solution brecciation process
Geological Society of America Bulletin (1966) 77 (8): 843-847
Index Terms/Descriptors
Latitude & Longitude
Abstract
A process of developing a breccia from evaporite rocks by simultaneous solution, subsidence, and evaporite flowage is described. The breccias studied come from cores from the Upper Devonian Leduc Formation, Alberta, Canada, and are dolomite clasts in a matrix of dolomite or anhydrite.
ISSN: 0016-7606
EISSN: 1943-2674
Coden: BUGMAF
Serial Title: Geological Society of America Bulletin
Serial Volume: 77
Serial Issue: 8
Title: The solution brecciation process
Author(s): Stanton, Robert J., Jr.
Pages: 843-847
Published: 1966
Text Language: English
Publisher: Geological Society of America (GSA),
Boulder, CO,
United States
Accession Number: 1966-003636
Categories: Sedimentary petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus.
N49°00'00" - N60°00'00", W120°00'00" - W110°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States
Update Code: 1966
