The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica

The mafic dyke is metamorphosed to amphibolite-facies and is calc-alkaline with intermediate SiO 2 (∼56%) and high Al 2O 3 and TiO 2 and is transitional between basaltic to andesitic compositions. The dyke has high Sr, Zr and Ba contents. The steep chon

Bibliographic Details
Main Authors: Grantham, Geoff H, Armstrong, Richard, Moyes, A.B.
Other Authors: Hanski, E., Mertanen, S., Ramo, T., Vuollo, J.
Format: Book Part
Language:unknown
Published: Taylor & Francis Group 2015
Subjects:
Dronning Maud Land
Sverdrupfjella
Roerkulten
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/26203
id ftanucanberra:oai:digitalcollections.anu.edu.au:1885/26203
record_format openpolar
spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/26203 2023-05-15T13:56:14+02:00 The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica Grantham, Geoff H Armstrong, Richard Moyes, A.B. Hanski, E. Mertanen, S. Ramo, T. Vuollo J. 2015-12-07T22:47:48Z http://hdl.handle.net/1885/26203 unknown Taylor & Francis Group Dyke Swarms: Time Markers of Crustal Evolution 1st Edition 9780415398992 http://hdl.handle.net/1885/26203 Book chapter 2015 ftanucanberra 2015-12-28T23:21:36Z The mafic dyke is metamorphosed to amphibolite-facies and is calc-alkaline with intermediate SiO 2 (∼56%) and high Al 2O 3 and TiO 2 and is transitional between basaltic to andesitic compositions. The dyke has high Sr, Zr and Ba contents. The steep chon Book Part Antarc* Antarctica Dronning Maud Land Australian National University: ANU Digital Collections Dronning Maud Land Sverdrupfjella ENVELOPE(0.583,0.583,-72.700,-72.700) Roerkulten ENVELOPE(0.333,0.333,-72.300,-72.300)
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
description The mafic dyke is metamorphosed to amphibolite-facies and is calc-alkaline with intermediate SiO 2 (∼56%) and high Al 2O 3 and TiO 2 and is transitional between basaltic to andesitic compositions. The dyke has high Sr, Zr and Ba contents. The steep chon
author2 Hanski, E.
Mertanen, S.
Ramo, T.
Vuollo
J.
format Book Part
author Grantham, Geoff H
Armstrong, Richard
Moyes, A.B.
spellingShingle Grantham, Geoff H
Armstrong, Richard
Moyes, A.B.
The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
author_facet Grantham, Geoff H
Armstrong, Richard
Moyes, A.B.
author_sort Grantham, Geoff H
title The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
title_short The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
title_full The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
title_fullStr The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
title_full_unstemmed The geology of a mafic dyke at Roerkulten, Sverdrupfjella, western Dronning Maud Land, Antarctica
title_sort geology of a mafic dyke at roerkulten, sverdrupfjella, western dronning maud land, antarctica
publisher Taylor & Francis Group
publishDate 2015
url http://hdl.handle.net/1885/26203
long_lat ENVELOPE(0.583,0.583,-72.700,-72.700)
ENVELOPE(0.333,0.333,-72.300,-72.300)
geographic Dronning Maud Land
Sverdrupfjella
Roerkulten
geographic_facet Dronning Maud Land
Sverdrupfjella
Roerkulten
genre Antarc*
Antarctica
Dronning Maud Land
genre_facet Antarc*
Antarctica
Dronning Maud Land
op_relation Dyke Swarms: Time Markers of Crustal Evolution
1st Edition
9780415398992
http://hdl.handle.net/1885/26203
_version_ 1766263610053492736

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