Constraining the Volume of Earth's Early Oceans With a Temperature‐Dependent Mantle Water Storage Capacity Model

Author:

Dong Junjie1ORCID,Fischer Rebecca A.1ORCID,Stixrude Lars P.23ORCID,Lithgow‐Bertelloni Carolina R.23ORCID

Affiliation:

1. Department of Earth and Planetary Sciences Harvard University Cambridge MA USA

2. Department of Earth Sciences University College London London UK

3. Department of Earth, Planetary, and Space Sciences University of California Los Angeles CA USA

Funder

Harvard University

FP7 Ideas: European Research Council

University of California, Los Angeles

Division of Earth Sciences

Publisher

American Geophysical Union (AGU)

Reference143 articles.

1. Abe Y. Ohtani E. Okuchi T. Righter K. &Drake M.(2000).Water in the Early Earth. InR. M.Canup&K.Righter(Eds.) Origin of the Earth and Moon(pp.413–433).University of Arizona Press.

2. Amante C. &Eakins B. W.(2009). ETOPO1 1 Arc‐Minute Global Relief Model: Procedures data sources and analysis. NOAA Technical Memorandum NESDIS NGDC‐24. National Geophysical Data Center NOAA.

3. H2O storage capacity of olivine at 5–8GPa and consequences for dehydration partial melting of the upper mantle

4. Why was flood volcanism on submerged continental platforms so common in the Precambrian?

5. Eclogites as palaeodynamic archives: Evidence for warm (not hot) and depleted (but heterogeneous) Archaean ambient mantle

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