Pore water evolution during sediment burial from isotopic and mineral chemistry of calcite, dolomite and siderite concretions

1986/10/01 by C. D. Curtis, C.D. Curtis, Max Coleman +3 · 12 citations
Chemistry · Earth and Planetary Sciences · #Alkalinity #Ankerite #Calcite #Carbonate #Carbonate minerals #Chemistry #Concretion #Diagenesis #Dolomite #Geochemistry #Geochemistry and Elemental Analysis #Geology #Geology and Paleoclimatology Research #Mineral #Mineralogy #Paleontology and Stratigraphy of Fossils #Pyrite #Rhodochrosite #Siderite

paper · doi:10.1016/0016-7037(86)90085-2

crossref issued 1986/10/01 · crossref published 1986/10/01 · crossref published-print 1986/10/01 · openalex publication_date 1986/10/01 · crossref created 2003/08/06 · crossref deposited 2019/03/16 · openalex created_date 2025/10/10 · crossref indexed 2026/07/07 · openalex updated_date 2026/07/07

Citations

• Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide

Cited by

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• Spherical and columnar, septarian, 18O‐depleted, calcite concretions from Middle–Upper Permian lacustrine siltstones in northern Mozambique: evidence for very early diagenesis and multiple fluids
• Significance of localized pore pressures to the genesis of septarian concretions
• Oxygen and carbon isotopic composition of marine carbonate concretions; an overview
• Isotopic constraints on growth conditions of multiphase calcite–pyrite–barite concretions in Carboniferous mudstones
• Microbially catalyzed dolomite formation: From near-surface to burial
• Anoxic and iron-rich seawater conditions facilitated reverse weathering: Evidence from the Mesoproterozoic siliceous rocks
• Concretion [wikipedia]