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Leucogranite intruding the South Tibetan Detachment in western Nepal: Implications for exhumation models in the Himalayas

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dc.contributor.authorCarosi, Rodolfo
dc.contributor.authorMontomoli, C
dc.contributor.authorRubatto, Daniela
dc.contributor.authorVisona, Dario
dc.date.accessioned2015-12-13T22:31:38Z
dc.date.issued2013
dc.date.updated2015-12-11T09:01:52Z
dc.description.abstractThe most popular models regarding the exhumation of the Greater Himalayan Sequence (GHS), such as extrusion, channel flow, critical taper and wedge extrusion, require prolonged activity of the two bounding shear zones and faults, the Main Central Thrust (
dc.identifier.issn0954-4879
dc.identifier.urihttp://hdl.handle.net/1885/75341
dc.publisherBlackwell Publishing Ltd
dc.sourceTerra Nova
dc.titleLeucogranite intruding the South Tibetan Detachment in western Nepal: Implications for exhumation models in the Himalayas
dc.typeJournal article
local.bibliographicCitation.issue6
local.bibliographicCitation.lastpage489
local.bibliographicCitation.startpage478
local.contributor.affiliationCarosi, Rodolfo, University of Torino
local.contributor.affiliationMontomoli, C, Universita di Pisa
local.contributor.affiliationRubatto, Daniela, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationVisona, Dario, University of Padova
local.contributor.authoruidRubatto, Daniela, u9909045
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040313 - Tectonics
local.identifier.absfor040303 - Geochronology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf5625xPUB4580
local.identifier.citationvolume25
local.identifier.doi10.1111/ter.12062
local.identifier.scopusID2-s2.0-84886753034
local.identifier.thomsonID000326180500008
local.type.statusPublished Version

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