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Montgomery‐Brown, E. K., Syracuse, E. M. (2015) Tremor‐genic slow slip regions may be deeper and warmer and may slip slower than non‐tremor‐genic regions. Geochemistry, Geophysics, Geosystems, 16 (10) 3593-3606 doi:10.1002/2015gc005895

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Reference TypeJournal (article/letter/editorial)
TitleTremor‐genic slow slip regions may be deeper and warmer and may slip slower than non‐tremor‐genic regions
JournalGeochemistry, Geophysics, Geosystems
AuthorsMontgomery‐Brown, E. K.Author
Syracuse, E. M.Author
Year2015 (October)Volume16
Issue10
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1002/2015gc005895Search in ResearchGate
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Mindat Ref. ID406786Long-form Identifiermindat:1:5:406786:7
GUID0
Full ReferenceMontgomery‐Brown, E. K., Syracuse, E. M. (2015) Tremor‐genic slow slip regions may be deeper and warmer and may slip slower than non‐tremor‐genic regions. Geochemistry, Geophysics, Geosystems, 16 (10) 3593-3606 doi:10.1002/2015gc005895
Plain TextMontgomery‐Brown, E. K., Syracuse, E. M. (2015) Tremor‐genic slow slip regions may be deeper and warmer and may slip slower than non‐tremor‐genic regions. Geochemistry, Geophysics, Geosystems, 16 (10) 3593-3606 doi:10.1002/2015gc005895
In(2015, October) Geochemistry, Geophysics, Geosystems Vol. 16 (10) American Geophysical Union (AGU)


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