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

Handy, M; Streit, J

Description

Dioritic 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.contributor.authorHandy, M
dc.contributor.authorStreit, J
dc.date.accessioned2015-12-13T23:22:33Z
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/91504
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.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.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume165
dc.date.issued1999
local.identifier.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub22263
local.type.statusPublished Version
local.contributor.affiliationHandy, M, Free University of Berlin
local.contributor.affiliationStreit, J, College of Physical and Mathematical Sciences, ANU
local.description.embargo2037-12-31
local.bibliographicCitation.startpage271
local.bibliographicCitation.lastpage286
local.identifier.doi10.1016/S0012-821X(98)00272-6
dc.date.updated2015-12-12T09:11:30Z
local.identifier.scopusID2-s2.0-0033557125
CollectionsANU Research Publications

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