Tectono‐Magmatic Evolution of the Southern Reykjanes Ridge, North Atlantic, From ∼11 M.y. to Present
Abstract Our understanding of the geological evolution of mid‐ocean ridges in response to tectonic reconfigurations and associated mantle processes is hampered by a lack of exploration in off‐axis areas. A notable exception is the Reykjanes Ridge, where multibeam bathymetry, magnetics, and gravity s...
I tiakina i:
| Ngā kaituhi matua: | , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Wiley
2025-01-01
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| Rangatū: | Geochemistry, Geophysics, Geosystems |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.1029/2024GC011847 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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