A regime diagram of mobile lid convection with plate-like behavior
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Rocky planets that are massive enough to allow solid-state convection in their mantles can exhibit a variety of geodynamic regimes at their surfaces, which may readily transition between different states over the thermal lifetime of the parent body.
“Rocky planets that are massive enough to allow solid-state convection in their mantles can exhibit a variety of geodynamic regimes at their surfaces, which may readily transition between different states over the thermal lifetime of the parent body”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Petersen et al., 2015
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Secular change and the onset of plate tectonics on Earth
Palin, R. M., Santosh, M., Cao, W., Li, S.-S., Hernández-Uribe, D., & Parsons, A. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103172 · Cited by 355 · see citing works
“Rocky planets that are massive enough to allow solid-state convection in their mantles can exhibit a variety of geodynamic regimes at their surfaces, which may readily transition between different states over the thermal lifetime of the parent body (Petersen et al., 2015).”
BackgroundExperimental and observational evidence for plume-induced subduction on Venus
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The subduction dichotomy of strong plates and weak slabs
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Self-citation
- Authors
- Petersen, R. I., Stegman, D. R., & Tackley, P. J.
- Affiliations
- University of California San Diego (US)
- ETH Zurich (CH)
- Corresponding author
- Petersen, Robert I.
- Venue
- Physics of The Earth and Planetary Interiors
- Publisher
- Elsevier BV
- Published
- 2015-04
- Volume
- 241
- Pages
- 65-76
- ISSN
- 0031-9201 (ISSN-L)
- OpenAlex
- W2054256846
- Cited by
- 5
- References
- 51
- Citations by year
- 2020: 1 · 2018: 1 · 2017: 2 · 2016: 1
- FWCI
- 1.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Physics of The Earth and Planetary Interiors (publishedVersion)
- Funders
- National Science Foundation (EAR-1255040, ACI-1053575)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- stagnant lid, plate tectonics, subduction, mantle convection, yield stress, temperature-dependent viscosity, regime diagram, Rayleigh number, plate strength
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