Cultural advice

The Australian National University acknowledges, celebrates and pays our respects to the Ngunnawal and Ngambri people of the Canberra region and to all First Nations Australians on whose traditional lands we meet and work, and whose cultures are among the oldest continuing cultures in human history.

Aboriginal and Torres Strait Islander peoples are advised that ANU Library collections may include images, names, voices, and other representations of deceased persons.

Material in the collection may contain terms, language or views that reflect the period in which the item was created and may be considered inappropriate today.

Evolution of Mafic Alkaline Melts Crystallized in the Uppermost Lithospheric Mantle: A Melt Inclusion Study of Olivine-Clinopyroxenite Xenoliths, Northern Hungary

Simple item page
dc.contributor.authorZajacz, Zoltan
dc.contributor.authorKovacs, Istvan
dc.contributor.authorSzabo, Csaba
dc.contributor.authorHalter, Werner
dc.contributor.authorPettke, Thomas
dc.date.accessioned2015-12-08T22:23:59Z
dc.date.issued2007
dc.date.updated2015-12-08T08:56:53Z
dc.description.abstractOlivine-clinopyroxenite xenoliths exhumed in alkali basalts (sensu lato) in the Nógrád-Gömör Volcanic Field (NGVF), northern Hungary, contain abundant silicate melt inclusions. Geothermobarometric calculations indicate that these xenoliths crystallize
dc.identifier.issn0022-3530
dc.identifier.urihttp://hdl.handle.net/1885/33108
dc.publisherOxford University Press
dc.sourceJournal of Petrology
dc.subjectKeywords: alkali basalt; alkaline rock; clinopyroxene; crystallization; igneous geochemistry; lithospheric structure; mafic rock; melt inclusion; olivine; petrogenesis; silicate melt; upper mantle; xenolith; Central Europe; Eurasia; Europe; Hungary Geochemistry; Nógrád-Gömör Volcanic Field; Pannonian Basin; Petrogenesis; Silicate melt inclusions
dc.titleEvolution of Mafic Alkaline Melts Crystallized in the Uppermost Lithospheric Mantle: A Melt Inclusion Study of Olivine-Clinopyroxenite Xenoliths, Northern Hungary
dc.typeJournal article
local.bibliographicCitation.issue5
local.bibliographicCitation.lastpage883
local.bibliographicCitation.startpage853
local.contributor.affiliationZajacz, Zoltan, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationKovacs, Istvan, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationSzabo, Csaba, Eotvos Lorand University
local.contributor.affiliationHalter, Werner, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationPettke, Thomas, University of Bern
local.contributor.authoruidKovacs, Istvan, u4178416
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040299 - Geochemistry not elsewhere classified
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.absfor040306 - Mineralogy and Crystallography
local.identifier.ariespublicationu9503261xPUB98
local.identifier.citationvolume48
local.identifier.doi10.1093/petrology/egm004
local.identifier.scopusID2-s2.0-34447645853
local.type.statusPublished Version

Downloads

Original bundle

Now showing 1 - 1 of 1
Thumbnail Image
Name:
01_Zajacz_Evolution_of_Mafic_Alkaline_2007.pdf
Size:
1.25 MB
Format:
Adobe Portable Document Format
Download

Collections

ANU Research Publications

DSpace software copyright © 2002-2026 LYRASIS