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-List Of Titles -U-Pb and Hf-isotope analyses of zircon from the Kundelungu kimberlites, D.R. Congo : implications for crustal evolution

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/20466

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Title
U-Pb and Hf-isotope analyses of zircon from the Kundelungu kimberlites, D.R. Congo : implications for crustal evolution
Related
Precambrian research, Vol. 156, Issue 3-4, p.195-225
DOI
10.1016/j.precamres.2007.04.002
Publisher
Elsevier
Date
2007
Author/Creator
Batumike, J. M
Author/Creator
O'Reilly, S. Y
Author/Creator
Griffin, W. L
Author/Creator
Belousova, E. A
Description
The Gungwania and Talala kimberlitic pipes on the Kundelungu Plateau (Katanga, SE Congo) have been used as drillholes, to obtain crustal zircons for a study of crustal evolution in the region and to constrain the age of the basement and the sedimentary provenance of the Katangan Supergroup. Two hundred and twenty-nine zircon grains were analysed for U–Pb ages and Hf-isotope compositions. Juvenile Mesoarchean (~3.4–3.3 Ga) crust in the region underwent recycling during Neoarchean and Paleoproterozoic time. The Paleoproterozoic event involved little production of juvenile crust, and this Paleoproterozoic crust was recycled during Mesoproterozoic and Neoproterozoic time. Both the Mesoproterozoic and Neoproterozoic were characterised by bimodal magmatism reflecting extension, linked with the break up of Rodinia and the opening of the Katangan basin, and the development of juvenile crust. Detailed studies of the external morphology of the zircons in different age groups suggest that the basement beneath the Kundelungu region is predominantly Paleoproterozoic in age; other zircon populations may be derived from the Katangan sediments. The absence of any zircons younger than 560 Ma supports deposition of the Biano Subgroup, which hosts the kimberlites, during the Pan-African Lufilian orogeny. The Archean Congo and Zimbabwe cratons, the Paleoproterozoic Ubendian Belt (Bangweulu Block), the Paleo-to-Mesoproterozoic Irumide Belt, the Mesoproterozoic Kibaran Belt and the Choma Kalomo Block may all have contributed material to the sediments of the Katangan Supergroup.
Description
31 page(s)
Subject Keyword
Zircon Geochronology, U-Pb dating, Hf isotopes, Crust evolution, Congo Craton, Kundelungu Kimberlite
Subject Keyword
zircon geochronology
Subject Keyword
zircon U–Pb dating
Subject Keyword
zircon Hf-isotopes
Subject Keyword
crust evolution
Subject Keyword
Congo craton
Subject Keyword
Kundelungu kimberlite
Resource Type
journal article
Organisation
Macquarie University. National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC)

Identifier
http://hdl.handle.net/1959.14/20466
Identifier
ISSN:0301-9268
Identifier
mq-rm-2007001078
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Precambrian research"
 
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