ReviewPhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2018
Magma oceans as a critical stage in the tectonic development of rocky planets.
Review in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2018. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.
What it found
Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.
The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
4 citing papers in PubMed.
- Insights into magma ocean dynamics from the transport properties of basaltic melt.Nature communications · 2022Article
- Vertically Resolved Magma Ocean-Protoatmosphere Evolution: HJournal of geophysical research. Planets · 2021Article
- A magma ocean origin to divergent redox evolutions of rocky planetary bodies and early atmospheres.Nature communications · 2020Article
- Earth dynamics and the development of plate tectonics.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018Article
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Authors and funding
2 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Magma oceans are a common result of the high degree of heating that occurs during planet formation. It is thought that almost all of the large rocky bodies in the Solar System went through at least one magma ocean phase. In this paper, we review some of the ways in which magma ocean models for the Earth, Moon and Mars match present-day observations of mantle reservoirs, internal structure and primordial crusts, and then we present new calculations for the oxidation state of the mantle produced during the magma ocean phase. The crystallization of magma oceans probably leads to a massive mantle overturn that may set up a stably stratified mantle. This may lead to significant delays or total prevention of plate tectonics on some planets. We review recent models that may help alleviate the mantle stability issue and lead to earlier onset of plate tectonics.This article is part of a discussion meeting issue 'Earth dynamics and the development of plate tectonics'.
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