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April 01, 1997
Selective dolomitization of Cambrian microbial carbonate deposits; a key to mechanisms and environments of origin Available to Purchase
Bosiljka Glumac;
Bosiljka Glumac
University of Tennessee, Department of Geological Sciences, Knoxville, TN, United States
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Bosiljka Glumac
University of Tennessee, Department of Geological Sciences, Knoxville, TN, United States
Kenneth R. Walker
Publisher: SEPM Society for Sedimentary Geology
First Online:
03 Mar 2017
Online ISSN: 1938-5323
Print ISSN: 0883-1351
GeoRef, Copyright 2004, American Geological Institute.
PALAIOS (1997) 12 (2): 98–110.
Article history
First Online:
03 Mar 2017
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CitationBosiljka Glumac, Kenneth R. Walker; Selective dolomitization of Cambrian microbial carbonate deposits; a key to mechanisms and environments of origin. PALAIOS 1997;; 12 (2): 98–110. doi: https://doi.org/10.2307/3515300
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Index Terms/Descriptors
- algae
- Appalachians
- arid environment
- bacteria
- basins
- biogenic structures
- calcification
- Cambrian
- carbonate platforms
- carbonatization
- classification
- coastal environment
- Conasauga Group
- Copper Ridge Dolomite
- correlation
- cyanobacteria
- Cyanophyta
- diagenesis
- dolomitization
- Iapetus
- intertidal environment
- Knox Group
- lagoonal environment
- laminations
- lithofacies
- lithostratigraphy
- marine environment
- Maynardville Limestone
- mechanism
- microfossils
- mineral composition
- North America
- paleoenvironment
- paleogeography
- Paleozoic
- petrography
- planar bedding structures
- Plantae
- reconstruction
- salinity
- sedimentary structures
- semi-arid environment
- shelf environment
- Southern Appalachians
- stromatolites
- Tennessee
- terrestrial environment
- thallophytes
- thrombolites
- United States
- Upper Cambrian
- eastern Tennessee
Latitude & Longitude
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