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Connolly, J.A.D., Kerrick, D.M. (2002) Metamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth. Earth and Planetary Science Letters, 204 (1) 61-74 doi:10.1016/s0012-821x(02)00957-3

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Reference TypeJournal (article/letter/editorial)
TitleMetamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth
JournalEarth and Planetary Science Letters
AuthorsConnolly, J.A.D.Author
Kerrick, D.M.Author
Year2002 (November)Volume204
Issue1
PublisherElsevier BV
DOIdoi:10.1016/s0012-821x(02)00957-3Search in ResearchGate
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Mindat Ref. ID376472Long-form Identifiermindat:1:5:376472:9
GUID0
Full ReferenceConnolly, J.A.D., Kerrick, D.M. (2002) Metamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth. Earth and Planetary Science Letters, 204 (1) 61-74 doi:10.1016/s0012-821x(02)00957-3
Plain TextConnolly, J.A.D., Kerrick, D.M. (2002) Metamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth. Earth and Planetary Science Letters, 204 (1) 61-74 doi:10.1016/s0012-821x(02)00957-3
In(2002, November) Earth and Planetary Science Letters Vol. 204 (1) Elsevier BV

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Kerrick, D.M., Connolly, J.A.D. (2001) Metamorphic devolatilization of subducted oceanic metabasalts: implications for seismicity, arc magmatism and volatile recycling. Earth and Planetary Science Letters, 189 (1) 19-29 doi:10.1016/s0012-821x(01)00347-8
Abers, G (2000) Hydrated subducted crust at 100–250 km depth. Earth and Planetary Science Letters, 176 (3) 323-330 doi:10.1016/s0012-821x(00)00007-8
(2002) Editorial Board. Earth and Planetary Science Letters, 204 (3) doi:10.1016/s0012-821x(02)01029-4
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Davis, E.E., Becker, K. (2002) Observations of natural-state fluid pressures and temperatures in young oceanic crust and inferences regarding hydrothermal circulation. Earth and Planetary Science Letters, 204 (1) 231-248 doi:10.1016/s0012-821x(02)00982-2
Ono, Shigeaki, Mibe, Kenji, Yoshino, Takashi (2002) Aqueous fluid connectivity in pyrope aggregates: water transport into the deep mantle by a subducted oceanic crust without any hydrous minerals. Earth and Planetary Science Letters, 203 (3) 895-903 doi:10.1016/s0012-821x(02)00920-2
Molina, J (2000) Carbonate stability and fluid composition in subducted oceanic crust: an experimental study on H2O–CO2-bearing basalts. Earth and Planetary Science Letters, 176 (3) 295-310 doi:10.1016/s0012-821x(00)00021-2
(2002) Editorial Board. Earth and Planetary Science Letters, 203 (3) doi:10.1016/s0012-821x(02)00987-1
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