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Magmatic evolution of the ultramafic--mafic Kharaelakh intrusion (Siberian Craton, Russia): insights from trace-element, U--Pb and Hf-isotope data on zircon

Authors :
Malitch, Kreshimir Nenadovitch
Belousova, Elena A.
Griffin, William L.
Badanina, Inna Yu
Pearson, Norman J.
Presnyakov, Sergey L.
Tuganova, Evgeniya V.
Source :
Contributions to Mineralogy and Petrology. June, 2010, Vol. 159 Issue 6, p753, 16 p.
Publication Year :
2010

Abstract

Byline: Kreshimir Nenadovitch Malitch (1), Elena A. Belousova (2), William L. Griffin (2), Inna Yu Badanina (1), Norman J. Pearson (2), Sergey L. Presnyakov (1), Evgeniya V. Tuganova (1) Keywords: Zircon; U--Pb age; Trace-elements; Hf-isotopes; Mafic and ultramafic rocks; Nd-isotopes; Magmatic evolution; Kharaelakh intrusion; Siberian Craton Abstract: The ultramafic--mafic Kharaelakh intrusion in the northwestern part of the Siberian Craton (Russia) hosts major economic platinum-group-element (PGE)--Cu--Ni sulphide deposits. In situ U--Pb, REE and Hf-isotope analyses of zircon from these rocks, combined with detailed study of crystal morphology and internal structure, identify four zircon populations. U--Pb ages of these populations cover a significant time span (from 347 +- 16 to 235.7 +- 6.1 Ma) suggesting multiple magmatic events that cluster around 350 and 250 Ma, being consistent with two recognised stages of active tectonism in the development of the Siberian Craton. The oldest zircon population, however, represents previously unknown stage of magmatic activity in the Noril'sk area. Epsilon-Hf values of +2.3 to +16.3 in the analysed zircons reflect a dominant role of mantle-derived magmas and suggest that juvenile mantle material was the main source for the ultramafic--mafic Kharaelakh intrusion. A significant range in initial 176.sup.Hf/ [.sup.177]Hf values, found in zircons that cluster around 250 Ma, indicate mixing between mantle and crustal magma sources. Our findings imply that economic intrusions hosting PGE--Cu--Ni deposits of the Noril'sk area have a far more complex geological history than is commonly assumed. Author Affiliation: (1) A.P. Karpinsky Russian Geological Research Institute, Sredny pr. 74, 199106, St. Petersburg, Russia (2) Department of Earth and Planetary Sciences, GEMOC ARC National Key Centre, Macquarie University, Sydney, NSW, 2109, Australia Article History: Registration Date: 05/10/2009 Received Date: 25/12/2008 Accepted Date: 05/10/2009 Online Date: 24/10/2009 Article note: Communicated by C. Ballhaus. Electronic supplementary material The online version of this article (doi: 10.1007/s00410-009-0452-z) contains supplementary material, which is available to authorized users.

Details

Language :
English
ISSN :
00107999
Volume :
159
Issue :
6
Database :
Gale General OneFile
Journal :
Contributions to Mineralogy and Petrology
Publication Type :
Academic Journal
Accession number :
edsgcl.229661157