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Félix, Gwenaëlle, Thomas, Nathalie (2004) Relation between dry granular flow regimes and morphology of deposits: formation of levées in pyroclastic deposits. Earth and Planetary Science Letters, 221 (1) 197-213 doi:10.1016/s0012-821x(04)00111-6

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Reference TypeJournal (article/letter/editorial)
TitleRelation between dry granular flow regimes and morphology of deposits: formation of levées in pyroclastic deposits
JournalEarth and Planetary Science Letters
AuthorsFélix, GwenaëlleAuthor
Thomas, NathalieAuthor
Year2004 (April 30)Volume221
Page(s)197-213Issue1
PublisherElsevier BV
DOIdoi:10.1016/s0012-821x(04)00111-6Search in ResearchGate
Mindat Ref. ID377952Long-form Identifiermindat:1:5:377952:5
GUIDc3a09c16-fefa-4263-8b92-e7471bab556d
Full ReferenceFélix, Gwenaëlle, Thomas, Nathalie (2004) Relation between dry granular flow regimes and morphology of deposits: formation of levées in pyroclastic deposits. Earth and Planetary Science Letters, 221 (1) 197-213 doi:10.1016/s0012-821x(04)00111-6
Plain TextFélix, Gwenaëlle, Thomas, Nathalie (2004) Relation between dry granular flow regimes and morphology of deposits: formation of levées in pyroclastic deposits. Earth and Planetary Science Letters, 221 (1) 197-213 doi:10.1016/s0012-821x(04)00111-6
In(2004, April) Earth and Planetary Science Letters Vol. 221 (1) Elsevier BV

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