Linking planetary-scale spatio-temporal trends in magma compositions and volcanic resurfacing on Mars
Martian volcanism exhibits two key global trends: magmas evolved from alkali- and silica-rich compositions in the Noachian epoch to alkali depleted mafic compositions in the Amazonian, while spatially, young (Amazonian) volcanic resurfacing is confine
Authors
- Olivier Bachmann (ORCID: https://orcid.org/0000-0003-2952-3465)
- J. W. Head (ORCID: https://orcid.org/0000-0003-2013-560X)
- Meredith Townsend (ORCID: https://orcid.org/0000-0001-8846-1466)
- Christian Huber (ORCID: https://orcid.org/0000-0001-6518-710X)
- Arka Chatterjee (ORCID: https://orcid.org/0009-0002-6997-1940)
Institutions
- Planetary Science Institute (US)
- Lehigh University (US)
- Institute of Geochemistry (CN)
Publication Details
- Published
- 2025-08-18
- DOI
- https://doi.org/10.22541/au.175433535.55280053/v2
- Primary Topic
- Planetary Science and Exploration
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- National Science Foundation
- Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung