Cited by 25Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisMineralogy and Gemology Studies

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Chapter 3. SOLID SOLUTIONS and SOLVI among METAMORPHIC CARBONATES with APPLICATIONS to GEOLOGIC THERMOBAROMETRY

Essene, Eric J.·1983·Carbonates

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Crossref · 10.1515/9781501508134-007

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  • Magnetite is thought to have formed from thermal decomposition of siderite at high temperatures, since siderite is typically stable only below 550 °C and has been seen to decompose at temperatures as low as 385 °C.

    “Magnetite is thought to have formed from thermal decomposition of siderite at high temperatures, since siderite is typically stable only below 550 °C (Essene 1983) and has been seen to decompose at temperatures as low as 385 °C (Gallagher et al. 1981).”

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Cited by 25

Metadata

Authors
Essene, E. J.
Corresponding author
Essene, Eric J.
Venue
Carbonates
Publisher
De Gruyter
Published
1983-12-31
Pages
77-96
OpenAlex
W4253116761
Cited by
25
References
0
Citations by year
2026: 1 · 2025: 1 · 2024: 1 · 2021: 1 · 2020: 1 · 2018: 1
FWCI
0.00
Type
book chapter
Language
en
Open access
closed
Locations
De Gruyter eBooks (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 › Geochemistry and Petrology › Mineralogy and Gemology Studies
Keywords
solid solutions, solvus, metamorphic pressure-temperature conditions

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