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Oligocene-Miocene back-thrusting in southern Mexico linked to the rapid subduction erosion of a large forearc block

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dc.contributor.authorKeppie, D Fraser
dc.contributor.authorHynes, A J
dc.contributor.authorLee, James K W
dc.contributor.authorNorman, Marc
dc.date.accessioned2015-12-10T23:26:24Z
dc.date.issued2012
dc.date.updated2016-02-24T08:47:41Z
dc.description.abstractBoth the timing and mechanism for the removal of a ∼150-250 km wide forearc block from southern Mexico during the Cenozoic are controversial. Principal competing hypotheses are (1) removal due to sinistral strike-slip shear, in which slow, diachronous r
dc.identifier.issn0278-7407
dc.identifier.urihttp://hdl.handle.net/1885/67742
dc.publisherAmerican Geophysical Union
dc.rightsAuthor/s retain copyrighten_AU
dc.sourceTectonics
dc.subjectKeywords: Average rate; Cenozoic; Continental lithosphere; Forearc; Late Oligocene; Me-xico; Miocene; Plutons; Shear zone; Subduction erosion; Upper mantle; Upper plate; Zircon age; Lithology; Mica; Zircon; Erosion; age determination; Cenozoic; continental arc; cru
dc.titleOligocene-Miocene back-thrusting in southern Mexico linked to the rapid subduction erosion of a large forearc block
dc.typeJournal article
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issue2
local.contributor.affiliationKeppie, D Fraser, Halifax
local.contributor.affiliationHynes, A J, Mc Gill University
local.contributor.affiliationLee, James K W, Queen's University
local.contributor.affiliationNorman, Marc, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidNorman, Marc, u4039549
local.description.notesImported from ARIES
local.identifier.absfor040300 - GEOLOGY
local.identifier.ariespublicationf5625xPUB1513
local.identifier.citationvolume31
local.identifier.doi10.1029/2011TC002976
local.identifier.scopusID2-s2.0-84859189222
local.identifier.thomsonID000301940700002
local.type.statusPublished Version

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