Bypassing and diachronous deposition from density currents: Evidence from a giant regressive bed form in the Poris ignimbrite, Tenerife, Canary Islands-Reference-Cited by-同舟云学术

Bypassing and diachronous deposition from density currents: Evidence from a giant regressive bed form in the Poris ignimbrite, Tenerife, Canary Islands

Published:2004 Issue:5 Volume:32 Page:445
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:Geol

Author:

Brown R.J.,Branney M.J.

Publisher

Geological Society of America

Subject

Geology

Reference14 articles.

1. A reappraisal of ignimbrite emplacement: progressive aggradation and changes from particulate to non-particulate flow during emplacement of high-grade ignimbrite

2. Giant bed from a sustained catastrophic density current flowing over topography: Acatlán ignimbrite, Mexico

3. The Quaternary pyroclastic succession of southeast Tenerife, Canary Islands: explosive eruptions, related caldera subsidence, and sector collapse

4. Stratigraphy of the Bandas del Sur Formation: an extracaldera record of Quaternary phonolitic explosive eruptions from the Las Cañadas edifice, Tenerife (Canary Islands)

5. The dynamics and thermodynamics of large ash flows

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