Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
South African Journal of Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

South African Journal of Geology; September 2006; v. 109; no. 3; p. 335-340; DOI: 10.2113/gssajg.109.3.335
© 2006 Geological Society of South Africa
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Cornell, D. H.
Right arrow Articles by Thomas, R. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Age and tectonic significance of the Banana Beach Gneiss, KwaZulu-Natal South Coast, South Africa

David H. Cornell

Department of Earth Sciences, University of Göteborg, Box 460, Göteborg Sweden. e-mail: cornell{at}gvc.gu.se

Robert J. Thomas

British Geological Survey, Keyworth, United Kingdom, e-mail: bthomas{at}bgs.ac.uk

A new ion probe U-Pb zircon date of 1065 ± 10 Ma has been obtained on the Banana Beach gneiss, Margate terrane, Natal sector of the Namaqua-Natal Metamorphic Province. The date is considered to represent a magmatic crystallization age. Zircon rims have been dated at 1021 ± 24 Ma, reflecting the regional high-grade metamorphic event. The magmatic date is younger than anticipated, as the gneiss was previously thought to be related to early arc-related magmatism during the early development of the Margate terrane, equivalent to the oldest ~1.24 to ~1.21 Ga arc- related intrusive and supracrustal rocks of the Mzumbe terrane to the north. The new date has rendered this interpretation untenable, as it shows that the gneiss is approximately coeval with granitoids and charnockites of the Oribi Gorge Suite, which have a within-plate signature. Published whole-rock geochemical analyses from the Banana Beach gneiss have been revisited and shown to have a mixed geochemical signature with respect to some elements. Thus the Banana Beach gneiss is now reinterpreted as a syn- to late-tectonic intrusion, possibly related to the within- plate Munster Metabasite Suite of the southern part of the Margate terrane. The differing geochemical signatures of the Banana Beach gneiss, Munster and Oribi Gorge Suites probably reflect different proportions of mantle versus crustal material derived from the thick lithosphere formed during the accretion of the province.




This article has been cited by other articles:


Home page
South African Journal of GeologyHome page
D. H. Cornell and A. Pettersson
Ion probe zircon dating of metasediments from the Areachap and Kakamas Terranes, Namaqua-Natal Province and the stratigraphic integrity of the Areachap Group
South African Journal of Geology, December 1, 2007; 110(4): 575 - 584.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Geological Society of South Africa