Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers
• Precise comparisons between turbidity current timing and potential triggers. • >4 ms−1 and 50 km runout flows can initiate without a major external trigger. • Turbidity current activity focussed during periods of enhanced sediment supply. • Rapid or sustained sediment supply alone may produce e...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Bailey, Lewis P. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2021 |
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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.] |
|---|---|
| Übergeordnetes Werk: |
volume:562 ; year:2021 ; day:15 ; month:05 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.epsl.2021.116845 |
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Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption |
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Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption |
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Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers |
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Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers |
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Bailey, Lewis P. |
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Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption |
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preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers |
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Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers |
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• Precise comparisons between turbidity current timing and potential triggers. • >4 ms−1 and 50 km runout flows can initiate without a major external trigger. • Turbidity current activity focussed during periods of enhanced sediment supply. • Rapid or sustained sediment supply alone may produce elevated pore pressures. • Which persist after deposition; minor perturbations can then cause slope failure. |
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• Precise comparisons between turbidity current timing and potential triggers. • >4 ms−1 and 50 km runout flows can initiate without a major external trigger. • Turbidity current activity focussed during periods of enhanced sediment supply. • Rapid or sustained sediment supply alone may produce elevated pore pressures. • Which persist after deposition; minor perturbations can then cause slope failure. |
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• Precise comparisons between turbidity current timing and potential triggers. • >4 ms−1 and 50 km runout flows can initiate without a major external trigger. • Turbidity current activity focussed during periods of enhanced sediment supply. • Rapid or sustained sediment supply alone may produce elevated pore pressures. • Which persist after deposition; minor perturbations can then cause slope failure. |
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Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers |
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Clare, Michael A. Rosenberger, Kurt J. Cartigny, Matthieu J.B. Talling, Peter J. Paull, Charles K. Gwiazda, Roberto Parsons, Daniel R. Simmons, Stephen M. Xu, Jingping Haigh, Ivan D. Maier, Katherine L. McGann, Mary Lundsten, Eve |
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