Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)
• Zoned garnet geochronology reveals durations and rates of Alpine subduction. • A ‘snapshot’ of the Alpine geothermal gradient at 45 Ma is presented. • Geometric calculations combined with petrochronology reconstruct Alpine subduction interface.
Autor*in: |
Dragovic, Besim [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2020 |
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Schlagwörter: |
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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.] |
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Übergeordnetes Werk: |
volume:547 ; year:2020 ; day:1 ; month:10 ; pages:0 |
Links: |
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DOI / URN: |
10.1016/j.epsl.2020.116446 |
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ELV050998749 |
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• Zoned garnet geochronology reveals durations and rates of Alpine subduction. • A ‘snapshot’ of the Alpine geothermal gradient at 45 Ma is presented. • Geometric calculations combined with petrochronology reconstruct Alpine subduction interface. |
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• Zoned garnet geochronology reveals durations and rates of Alpine subduction. • A ‘snapshot’ of the Alpine geothermal gradient at 45 Ma is presented. • Geometric calculations combined with petrochronology reconstruct Alpine subduction interface. |
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• Zoned garnet geochronology reveals durations and rates of Alpine subduction. • A ‘snapshot’ of the Alpine geothermal gradient at 45 Ma is presented. • Geometric calculations combined with petrochronology reconstruct Alpine subduction interface. |
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