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

Date

Authors

Zajacz, Zoltan

Kovacs, Istvan

Szabo, Csaba

Halter, Werner

Pettke, Thomas

Publisher

Oxford University Press

Abstract

Olivine-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

Keywords

Keywords: 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

URI

http://hdl.handle.net/1885/33108

Collections

ANU Research Publications

Source

Journal of Petrology

Type

Journal article

DOI

10.1093/petrology/egm004

Restricted until

2037-12-31

Downloads

File

Description

01_Zajacz_Evolution_of_Mafic_Alkaline_2007.pdf (1.25 MB)

abcd