Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/13244
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dc.contributor.authorTalusani, Reddy VRen
dc.contributor.authorAshley, Paulen
local.source.editorEditor(s): Solomon Buckman and Phillip L Blevinen
dc.date.accessioned2013-08-15T17:04:00Z-
dc.date.issued2010-
dc.identifier.citationNew England Orogen 2010: Proceedings of a conference held at the University of New England, Armidale, New South Wales, Australia, November 2010, p. 304-307en
dc.identifier.isbn9781921597244en
dc.identifier.urihttps://hdl.handle.net/1959.11/13244-
dc.description.abstractMagmatic activity frequently accompanies continental rifting, and is generally considered to be the consequence of adiabatic decompression melting of the convecting mantle as it upwells beneath the thinned lithosphere (McKenzie and Bickle, 1988). The volume and composition of the magmas generated during rifting have been shown to be directly related to the degree and duration of extension, the temperature of the underlying asthenospheric mantle. Extension and thinning of the lithosphere cause adiabatic decompression melting of the asthenospheric mantle. Additionally, melting within the lithospheric mantle may occur through direct partial melting of metasomatised layers, resulting in magmas that are enriched in incompatible trace elements (McKenzie, 1989). Small-volume mafic alkaline volcanism occurs in many geologically recent areas of continental extension. The geochemistry of primitive volcanic rocks can be used to model partial melting conditions and assess relative contributions of lithospheric and asthenospheric mantle melts. ... This study focuses on the chemical and isotopic study of the late Pleistocene Barambah basalts from southeast Queensland, to evaluate their mantle source characteristics and evolution.en
dc.languageenen
dc.publisherUniversity of New Englanden
dc.relation.ispartofNew England Orogen 2010: Proceedings of a conference held at the University of New England, Armidale, New South Wales, Australia, November 2010en
dc.titleThe petrogenesis of late Pleistocene Barambah basalts from southeast Queensland, Australiaen
dc.typeConference Publicationen
dc.relation.conferenceNEO 2010: New England Orogen Conferenceen
dc.subject.keywordsIgneous and Metamorphic Petrologyen
local.contributor.firstnameReddy VRen
local.contributor.firstnamePaulen
local.subject.for2008040304 Igneous and Metamorphic Petrologyen
local.subject.seo2008849999 Mineral Resources (excl. Energy Resources) not elsewhere classifieden
local.profile.schoolSchool of Environmental and Rural Scienceen
local.profile.emailvtalusan@hotmail.comen
local.profile.emailpashley@une.edu.auen
local.output.categoryE2en
local.record.placeauen
local.record.institutionUniversity of New Englanden
local.identifier.epublicationsrecordune-20110204-120316en
local.date.conference16th - 19th November, 2010en
local.conference.placeArmidale, Australiaen
local.publisher.placeArmidale, Australiaen
local.format.startpage304en
local.format.endpage307en
local.contributor.lastnameTalusanien
local.contributor.lastnameAshleyen
dc.identifier.staffune-id:rtalusanen
dc.identifier.staffune-id:pashleyen
local.profile.roleauthoren
local.profile.roleauthoren
local.identifier.unepublicationidune:13456en
dc.identifier.academiclevelAcademicen
dc.identifier.academiclevelAcademicen
local.title.maintitleThe petrogenesis of late Pleistocene Barambah basalts from southeast Queensland, Australiaen
local.output.categorydescriptionE2 Non-Refereed Scholarly Conference Publicationen
local.relation.urlhttps://sites.google.com/site/newenglandorogenconference/past-new-england-conference-volumesen
local.relation.urlhttp://trove.nla.gov.au/version/51153861en
local.conference.detailsNEO 2010: New England Orogen Conference, Armidale, Australia, 16th - 19th November, 2010en
local.search.authorTalusani, Reddy VRen
local.search.authorAshley, Paulen
local.uneassociationUnknownen
local.year.published2010en
local.date.start2010-11-16-
local.date.end2010-11-19-
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