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Stable isotope composition and volume of Early Archaean oceans
Emily Catherine Pope,
Minik Thorleif Rosing
, Dennis K. Bird
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Dive into the research topics of 'Stable isotope composition and volume of Early Archaean oceans'. Together they form a unique fingerprint.
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Keyphrases
Archean Ocean
100%
Early Archean
100%
Stable Isotope Ratios
100%
Serpentinite
100%
Oceanic Crust
66%
Hydrogen Isotopes
66%
Seawater
66%
Earth System
66%
VSMOW
66%
Archean Seawater
33%
Hydrogen Escape
33%
Chert
33%
Oxygen Isotope Analysis
33%
Lizardite
33%
Archean
33%
Earth Sciences
33%
West Greenland
33%
Diagenesis
33%
Isotope Variability
33%
Science Review
33%
Ocean Floor
33%
Mass Balance
33%
Continental Crust
33%
Isua Supracrustal Belt
33%
Carbonate
33%
Atmospheric Methane
33%
Elevated Temperature
33%
Isotopic Exchange
33%
Isua
33%
Volatile Fluxes
33%
Hydrothermal Fluids
33%
Geologic Time
33%
Oxygen Isotopes
33%
Hydrogen Loss
33%
Methanogenesis
33%
Low Strain
33%
Earth and Planetary Sciences
Serpentinite
100%
Stable Isotope
100%
Continent
66%
Hydrogen Isotope
66%
Atmospherics
66%
Oceanic Crust
66%
Chemical Element
66%
Chert
33%
Earth Science
33%
Methane
33%
Diagenesis
33%
Precambrian
33%
Isotope Ratios
33%
Methanogenesis
33%
Hydrothermal Fluid
33%
Oxygen 18
33%
Continental Crust
33%
Sea Bed
33%
Greenland
33%
Ocean Temperature
33%
Lizardite
33%