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Secular variation of calcium carbonate mineralogy; an evaluation of ooid and micrite chemistries
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The textures of ooids appear to vary during Phanerozoic time.
“Although still somewhat controversial (e.g., Bates and Brand, 1990), the textures of ooids appear to vary during Phanerozoic time.”
From Evolution of Sedimentary Rocks (2014) · cites this paper as Bates and Brand, 1990
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References 80 · Cited by 32
Research works printed but not linked: 84
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Metadata
- Authors
- Bates, N. R., & Brand, U.
- Affiliations
- Brock University (CA)
- Venue
- Geologische Rundschau
- Published
- 1990-02
- Volume
- 79
- Issue
- 1
- Pages
- 27-46
- ISSN
- 1437-3254 (ISSN-L)
- 0016-7835
- 1437-3262
- OpenAlex
- W2021540698
- Cited by
- 32
- References
- 80
- Citations by year
- 2024: 1 · 2022: 2 · 2019: 1 · 2018: 2 · 2017: 1 · 2013: 1
- FWCI
- 2.66
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- International Journal of Earth Sciences (publishedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- Funders
- Natural Sciences and Engineering Research Council of Canada
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Keywords
- ooids, micrite, aragonite, calcite, calcite seas, Tournaisian, Lower Carboniferous, diagenesis, Mg/Ca ratio, atmospheric pCO2, shallow-water carbonates
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