Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9548
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dc.contributor.authorallPersaud, P.; Caltech, Cal. Polyen
dc.contributor.authorallDi Luccio, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallClayton, R.; Caltechen
dc.date.accessioned2015-04-20T08:35:11Zen
dc.date.available2015-04-20T08:35:11Zen
dc.date.issued2015-03en
dc.identifier.urihttp://hdl.handle.net/2122/9548en
dc.description.abstractRayleigh wave tomography provides images of the shallow mantle shear wave velocity structure beneath the Gulf of California. Low-velocity zones (LVZs) are found on axis between 26 and 50 km depth beneath the Guaymas Basin but mostly off axis under the other rift basins, with the largest feature underlying the Ballenas Transform Fault. We interpret the broadly distributed LVZs as regions of partial melting in a solid mantle matrix. The pathway for melt migration and focusing is more complex than an axis-centered source aligned above a deeper region of mantle melt and likely reflects the magmatic evolution of rift segments. We also consider the existence of solid lower continental crust in the Gulf north of the Guaymas Basin, where the association of the LVZs with asthenospheric upwelling suggests lateral flow assisted by a heat source. These results provide key constraints for numerical models of mantle upwelling and melt focusing in this young oblique rift.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries/42 (2015)en
dc.relation.isversionofhttp://onlinelibrary.wiley.com/doi/10.1002/2015GL063420/abstracten
dc.subjectLow velocities in the Gulf upper mantle are interpreted as partial meltingen
dc.subjectPartial melting under the Guaymas Basin and off axis of the other rift basinsen
dc.subjectLower crustal flow assisted by heat source in N Gulf near mantle upwellingen
dc.titleRayleigh wave dispersion measurements reveal low-velocity zones beneath the new crust in the Gulf of Californiaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1766–1774en
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.03. Mantle and Core dynamicsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.identifier.doi10.1002/2015GL063420en
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dc.description.obiettivoSpecifico1T. Geodinamica e interno della Terraen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.issn0094-8276en
dc.relation.eissn1944-8007en
dc.contributor.authorPersaud, P.en
dc.contributor.authorDi Luccio, F.en
dc.contributor.authorClayton, R.en
dc.contributor.departmentCaltech, Cal. Polyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentCaltechen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptCaltech-
crisitem.author.orcid0000-0003-3462-7023-
crisitem.author.orcid0000-0002-9924-3736-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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