Warren, C. J.; Grujic, D.; Kellet, D. A.; Cottle, J.; Jamieson, R. A. and Ghalley, K. S.
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|DOI (Digital Object Identifier) Link:||https://doi.org/10.1029/2010TC002738|
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Rocks metamorphosed to high temperatures and/or high pressures are rare across the Himalayan orogen, where peak metamorphic conditions recorded in the exposed metamorphic core, the Greater Himalayan Sequence (GHS), are generally at middle to upper amphibolite-facies. However, mafic garnet-clinopyroxene assemblages exposed at the highest structural levels in Bhutan, eastern Himalaya, preserve patchy textural evidence for early eclogite-facies conditions, overprinted by granulite-facies conditions. Monazite hosted within the leucosome of an associated granulite-facies orthopyroxene-bearing felsic gneiss yields LA-MC-ICP-MS U-Th-Pb ages of 13.9 ?? 0.3 Ma. Monazite associated with sillimanite-grade metamorphism in granulite-hosting migmatitic gneisses yields U-Th-Pb rim ages between 15.4 ± 0.8 Ma and 13.5 ± 0.5 Ma and core ages of ca. 550 Ma. Monazite associated with sillimanite-grade metamorphism in gneiss at structurally lower levels yields U-Pb rim ages of 21-17 Ma and core ages of 600-500 Ma. These data are consistent with Miocene exhumation of GHS material from a variety of crustal depths at different times along the Himalayan orogen. We propose that tectonic forcing over an incoming Indian crustal ramp is a viable mechanism for exhumation of lower crustal granulitised eclogites in Bhutan.
|Item Type:||Journal Article|
|Copyright Holders:||2011 the American Geophysical Union|
|Keywords:||Bhutan; U-Pb geochronology; Himalayas; granulite; monazite|
|Academic Unit/School:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Clare Warren|
|Date Deposited:||11 Jan 2011 16:29|
|Last Modified:||04 Dec 2016 03:41|
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