3He evidence for fluid transfer and continental hydration above a flat slab
• Mantle helium in Peruvian springs evidence for slab-to-lithosphere fluid transfer. • Flat slabs lead to hydration and metasomatism in overlying continental lithosphere. • Helium isotope ratios inform of fluid transit times through the crust. • Crustal structures and slab morphology influence flow...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hiett, Coleman D. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption - Kılıç Depren, Serpil ELSEVIER, 2022, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:556 ; year:2021 ; day:15 ; month:02 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.epsl.2020.116722 |
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• Mantle helium in Peruvian springs evidence for slab-to-lithosphere fluid transfer. • Flat slabs lead to hydration and metasomatism in overlying continental lithosphere. • Helium isotope ratios inform of fluid transit times through the crust. • Crustal structures and slab morphology influence flow rates through the crust. • Dehydration and/or melting of lithospheric mantle below northern Altiplano Plateau. |
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• Mantle helium in Peruvian springs evidence for slab-to-lithosphere fluid transfer. • Flat slabs lead to hydration and metasomatism in overlying continental lithosphere. • Helium isotope ratios inform of fluid transit times through the crust. • Crustal structures and slab morphology influence flow rates through the crust. • Dehydration and/or melting of lithospheric mantle below northern Altiplano Plateau. |
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• Mantle helium in Peruvian springs evidence for slab-to-lithosphere fluid transfer. • Flat slabs lead to hydration and metasomatism in overlying continental lithosphere. • Helium isotope ratios inform of fluid transit times through the crust. • Crustal structures and slab morphology influence flow rates through the crust. • Dehydration and/or melting of lithospheric mantle below northern Altiplano Plateau. |
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| doi_str |
10.1016/j.epsl.2020.116722 |
| up_date |
2024-07-06T16:47:21.724Z |
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