UCL  IRIS
Institutional Research Information Service
UCL Logo
Please report any queries concerning the funding data grouped in the sections named "Externally Awarded" or "Internally Disbursed" (shown on the profile page) to your Research Finance Administrator. Your can find your Research Finance Administrator at http://www.ucl.ac.uk/finance/research/post_award/post_award_contacts.php by entering your department
Please report any queries concerning the student data shown on the profile page to:

Email: portico-services@ucl.ac.uk

Help Desk: http://www.ucl.ac.uk/ras/portico/helpdesk
Publication Detail
Petrology and geochemistry of granulite xenoliths from Udachnaya and Komsomolskaya kimberlite pipes, Siberia
  • Publication Type:
    Journal article
  • Publication Sub Type:
    Journal Article
  • Authors:
    Koreshkova MY, Downes H, Levsky LK, Vladykin NV
  • Publication date:
    01/10/2011
  • Pagination:
    1857, 1885
  • Journal:
    Journal of Petrology
  • Volume:
    52
  • Issue:
    10
  • Status:
    Published
  • Print ISSN:
    0022-3530
Abstract
Lower crustal xenoliths from the Udachnaya and Komsomolskaya kimberlite pipes in Siberia are mainly meta-igneous mafic garnet granulites, with subordinate feldspar-rich garnet granulites. Pressure and temperature estimates are interpreted as the conditions in the lower crust at the time of the last granulite-facies metamorphic event (800-890°C) followed by cooling to 610-720°C with a pressure decrease from 1·2 to 0·8 GPa. Most of the xenoliths show minor alteration. Leaching experiments demonstrate that their isotopic, major and trace element compositions have been affected by interaction not only with the host kimberlite but also with a fluid mobilized from local sedimentary country rocks. To obtain unambiguous compositional data we have calculated the composition of selected samples using modal analyses, electron microprobe and laser ablation inductively coupled plasma mass spectrometry data for constituent minerals. The reconstructed protoliths of most of the xenoliths were Fe-tholeiites of intraplate affinity, similar to some Archean basalts, whereas the others show characteristics of subduction-related magmas. However, the mafic granulites are strongly depleted in Rb, Th and U, which were removed by a small-degree partial melt. A protolith age of c. 3 Ga is supported by a disturbed Sm-Nd isochron, Nd and Hf model ages, and published U-Pb ages of zircon cores. © The Author 2011. Published by Oxford University Press. All rights reserved.
Publication data is maintained in RPS. Visit https://rps.ucl.ac.uk
 More search options
UCL Researchers
Author
Dept of Earth Sciences
University College London - Gower Street - London - WC1E 6BT Tel:+44 (0)20 7679 2000

© UCL 1999–2011

Search by