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Mechanics and mechanisms of magmatic underplating: inferences from mafic veins in deep crustal mylonite

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dc.contributor.authorHandy, M
dc.contributor.authorStreit, J
dc.date.accessioned2015-12-13T23:22:33Z
dc.date.issued1999
dc.date.updated2015-12-12T09:11:30Z
dc.description.abstractDioritic to gabbro-dioritic veins with extreme length to width ratios (>1000:1) are localized along an amphibolite facies shear zone (the CMB Line) between exposed segments of originally middle and lower continental crust (Strona-Ceneri and Ivrea-Verbano
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/91504
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: deformation; mylonite; shear zone; underplating; Italy Brittle materials; Magmas; Mylonites; Shear zones; Underplating; Viscous materials
dc.titleMechanics and mechanisms of magmatic underplating: inferences from mafic veins in deep crustal mylonite
dc.typeJournal article
local.bibliographicCitation.lastpage286
local.bibliographicCitation.startpage271
local.contributor.affiliationHandy, M, Free University of Berlin
local.contributor.affiliationStreit, J, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidStreit, J, u3748643
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub22263
local.identifier.citationvolume165
local.identifier.doi10.1016/S0012-821X(98)00272-6
local.identifier.scopusID2-s2.0-0033557125
local.type.statusPublished Version

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