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Evaluation of proposed precipitation mechanisms for Mississippi Valley-type deposits
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The new model naturally explains the growth of late-stage calcite, a feature that had long been puzzling from the perspective of the prevailing theory of burial dolomitization.
“The new model thus naturally explains a feature-growth of so-called late-stage calcite-that had long been puzzling (Spirakis and Heyl, 1995) from the perspective of the prevailing theory of burial dolomitization.”
From Self-accelerating dolomite-for-calcite replacement: Self-organized dynamics of burial dolomitization and associated mineralization (2011) · cites this paper as Spirakis and Heyl, 1995
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Cited by
Sorted by citations
Merino, E., & Canals, A. (2011) · American Journal of Science · doi:10.2475/07.2011.01 · Cited by 100
Metadata
- Authors
- Spirakis, C. S., & Heyl, A. V.
- Affiliations
- United States Geological Survey (US)
- Venue
- Ore Geology Reviews
- Publisher
- Elsevier BV
- Published
- 1995-08
- Volume
- 10
- Issue
- 1
- Pages
- 1-17
- ISSN
- 0169-1368 (ISSN-L)
- OpenAlex
- W2021963052
- Cited by
- 30
- References
- 0
- Citations by year
- 2026: 3 · 2025: 1 · 2024: 1 · 2023: 2 · 2022: 2 · 2020: 1 · 2018: 2 · 2017: 1 · 2016: 1 · 2015: 1 · 2014: 1 · 2013: 1 · 2012: 1
- FWCI
- 0.00
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Ore Geology Reviews (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- Mississippi Valley-type deposits, sulfate reduction, solution blending, organic acids
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