at Google ScholarTitle data
Paul, Jyotirmoy ; Conrad, Clinton P. ; Becker, Thorsten W. ; Ghosh, Attreyee:
Convective Self-Compression of Cratons and the Stabilization of Old Lithosphere.
In: Geophysical Research Letters.
Vol. 50
(2023)
Issue 4
.
- e2022GL101842.
ISSN 1944-8007
DOI: https://doi.org/10.1029/2022GL101842
Abstract in another language
Abstract Despite being exposed to convective stresses for much of the Earth's history, cratonic roots appear capable of resisting mantle shearing. This tectonic stability can be attributed to the neutral density and higher strength of cratons. However, the excess thickness of cratons and their higher viscosity amplify coupling to underlying mantle flow, which could be destabilizing. To investigate the stresses that a convecting mantle exerts on cratons that are both strong and thick, we developed instantaneous global spherical numerical models that incorporate present-day geoemetry of cratons within active mantle flow. Our results show that mantle flow is diverted downward beneath thick and viscous cratonic roots, giving rise to a ring of elevated and inwardly-convergent tractions along a craton's periphery. These tractions induce regional compressive stress regimes within cratonic interiors. Such compression could serve to stabilize older continental lithosphere against mantle shearing, thus adding an additional factor that promotes cratonic longevity.
Further data
| Item Type: | Article in a journal |
|---|---|
| Refereed: | Yes |
| Keywords: | craton; numerical model; mantle convection; geodynamics |
| Institutions of the University: | Research Institutions > Central research institutes > Bavarian Research Institute of Experimental Geochemistry and Geophysics - BGI Research Institutions Research Institutions > Central research institutes |
| Result of work at the UBT: | Yes |
| DDC Subjects: | 500 Science > 550 Earth sciences, geology |
| Date Deposited: | 08 Jun 2024 21:00 |
| Last Modified: | 08 Jun 2024 21:00 |
| URI: | https://eref.uni-bayreuth.de/id/eprint/89711 |