Formation of Replacement Dolomite in the Latemar Carbonate Buildup, Dolomites, Northern Italy: Part 2. Origin of the Dolomitizing Fluid and the Amount and Duration of Fluid Flow
- ASU Author/Contributor (non-ASU co-authors, if there are any, appear on document)
- Sarah K. Carmichael Ph.D., Assistant Professor of Geology (Creator)
- Institution
- Appalachian State University (ASU )
- Web Site: https://library.appstate.edu/
Abstract: Replacement dolomite in the Latemar carbonate buildup developed when limestone was infiltrated by reactive fluid. Minor-element, trace-element, and oxygen and carbon isotope compositions of dolomite and precursor limestone constrain the origin of the fluid and fundamental aspects of the flow… [See article for complete abstract]
Formation of Replacement Dolomite in the Latemar Carbonate Buildup, Dolomites, Northern Italy: Part 2. Origin of the Dolomitizing Fluid and the Amount and Duration of Fluid Flow
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Created on 11/4/2010
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Additional Information
- Publication
- Carmichael, Sarah K., and Ferry, John M., 2008, Formation of replacement dolomite in the Latemar carbonate buildup, Dolomites, northern Italy: Part 2. Origin of the dolomitizing fluid and the amount and duration of fluid flow. American Journal of Science, v. 308, no. 8, p. 885-904. Archived in NC DOCKS with permission of the editor. (ISSN: 0002-9599) Oct. 2008 DOI 10.2475/08.2008.01
- Language: English
- Date: 2008