Intraplate volcanism driven by slab-plume interaction: Numerical modeling and its application to the Eifel, Massif Central and Hainan volcanic areas
Intraplate volcanism has long been linked with deep mantle plumes. However, recent studies showed that intraplate magmatism can originate from transition zone dynamics, where lower-mantle plumes might be ponding, creating a Thermal Boundary Layer (TBL
Authors
- Anne Glerum (ORCID: https://orcid.org/0000-0002-9481-1749)
- Michaël Pons (ORCID: https://orcid.org/0000-0002-4785-5570)
- Bernhard Steinberger (ORCID: https://orcid.org/0000-0002-3643-3049)
- Y. Li (ORCID: https://orcid.org/0000-0003-0361-2152)
- Eline Le Breton (ORCID: https://orcid.org/0000-0003-0577-9853)
- Sascha Brune (ORCID: https://orcid.org/0000-0003-4985-1810)
Institutions
- GFZ Helmholtz Centre for Geosciences (DE)
- Université de Rennes (FR)
Publication Details
- Published
- 2025-08-29
- DOI
- https://doi.org/10.22541/essoar.175647574.44434700/v1
- Primary Topic
- Geological Modeling and Analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.00