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Contact metamorphism of the Tethyan Sedimentary Sequence, Upper Mustang region, west-central Nepal

Published online by Cambridge University Press:  24 April 2020

Iva Lihter Open the ORCID record for Iva Lihter [Opens in a new window] ,
Kyle P. Larson ,
Sudip Shrestha ,
John M. Cottle  and
Alex D. Brubacher
Iva Lihter*
Affiliation:
Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, Kelowna, BCV1V 1V7, Canada
Kyle P. Larson
Affiliation:
Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, Kelowna, BCV1V 1V7, Canada
Sudip Shrestha
Affiliation:
Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, Kelowna, BCV1V 1V7, Canada Present address: Fipke Laboratory for Trace Element Research, University of British Columbia Okanagan, Kelowna, BC V1V 1V7, Canada
John M. Cottle
Affiliation:
Department of Earth Science, University of California, Santa Barbara, CA93106–9630, USA
Alex D. Brubacher
Affiliation:
Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, Kelowna, BCV1V 1V7, Canada Present address: Newmont Corporation, Whitehorse, YT Y1A 0G1, Canada
*
Author for correspondence: Iva Lihter, Email: iva.lihter@alumni.ubc.ca
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Abstract

The Upper Mustang region of west-central Nepal contains exposures of metamorphosed Tethyan Sedimentary Sequence rocks that have been interpreted to reflect either contact metamorphism related to the nearby Mugu pluton or regional metamorphism associated with the North Himalayan domes. New monazite geochronology results show that the Mugu leucogranite crystallized at c. 21.3 Ma, while the dominant monazite age peaks from the surrounding garnet ± staurolite ± sillimanite schists range between c. 21.7 and 19.4 Ma, generally decreasing in age away from the pluton. Metamorphic temperature estimates based on Ti-in-biotite and garnet–biotite thermometry are highest in the specimens closest to the pluton (648 ± 24°C and 615 ± 25°C, respectively) and lowest in those furthest away (578 ± 24°C and 563 ± 25°C, respectively), while pressure estimates are all within uncertainty of one another, averaging 5.0 ± 0.5 kbar. These results are interpreted to be consistent with contact metamorphism of the rocks in proximity to the Mugu pluton, which was emplaced at c. 18 ± 2 km depth after local movement across the South Tibetan detachment system had ceased. While this new dataset helps to characterize the metamorphic rocks of the Tethyan Sedimentary Sequence and provides new constraints on the thickness of the upper crust, it also emphasizes the importance of careful integration of metamorphic conditions and inferred processes that may affect interpretation of currently proposed Himalayan models.

Keywords

contact metamorphismHimalayaMustangthermobarometrymonazite petrochronology
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 11 , November 2020 , pp. 1917 - 1932
Copyright
© Cambridge University Press 2020

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