The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya

A garnet-bearing schist from the southernmost such exposure along the Himalaya in east central Nepal records prograde metamorphism at 32.4 ​± ​0.3 ​Ma. Phase equilibria modelling, combined with Ti-in-biotite and quartz c-axis thermometry, outline a tight-to-hairpin pressure-temperature (P-T) path ex...

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Main Authors: Kyle P. Larson, Sudip Shrestha, Mathieu Soret, Matthijs Smit
Format: Article
Language:English
Published: Elsevier 2022-03-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S167498712030181X
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author Kyle P. Larson
Sudip Shrestha
Mathieu Soret
Matthijs Smit
author_facet Kyle P. Larson
Sudip Shrestha
Mathieu Soret
Matthijs Smit
author_sort Kyle P. Larson
collection DOAJ
description A garnet-bearing schist from the southernmost such exposure along the Himalaya in east central Nepal records prograde metamorphism at 32.4 ​± ​0.3 ​Ma. Phase equilibria modelling, combined with Ti-in-biotite and quartz c-axis thermometry, outline a tight-to-hairpin pressure-temperature (P-T) path extending from ~515 ​°C and 5.5 ​kbar to peak conditions at ~575 ​°C and 7 ​kbar followed by deformation during the retrograde phase at 480–515 ​°C and 6–7 ​kbar. The new geochronology data place an upper bound on the evolution of metamorphism and deformation in the frontal-most part of the Himalaya, which lasted until 17.5 ​Ma, as indicated by previously published 40Ar/39Ar data. The P-T-time data from this part of the Himalaya, as well as that from more hinterland-ward portions of the orogen, outline a progressive, stepwise, commonly out-of-sequence evolution. Further data from along the orogen indicates that this evolution is not a local phenomenon, but instead characterizes the tectonics of this system as a whole.
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spelling doaj.art-05d78d94456b4f76867d3c1e217f8de72023-09-02T13:09:05ZengElsevierGeoscience Frontiers1674-98712022-03-01132101057The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the HimalayaKyle P. Larson0Sudip Shrestha1Mathieu Soret2Matthijs Smit3Department of Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, 3247 University Way, Kelowna, BC V1V 1V7, Canada; Corresponding author.Department of Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, 3247 University Way, Kelowna, BC V1V 1V7, CanadaDepartment of Earth, Environmental and Geographic Sciences, University of British Columbia Okanagan, 3247 University Way, Kelowna, BC V1V 1V7, CanadaDepartment of Earth, Ocean and Atmospheric Sciences, University of British Columbia Vancouver, 2020-2207 Main Mall, Vancouver, BC V6T 1Z4, CanadaA garnet-bearing schist from the southernmost such exposure along the Himalaya in east central Nepal records prograde metamorphism at 32.4 ​± ​0.3 ​Ma. Phase equilibria modelling, combined with Ti-in-biotite and quartz c-axis thermometry, outline a tight-to-hairpin pressure-temperature (P-T) path extending from ~515 ​°C and 5.5 ​kbar to peak conditions at ~575 ​°C and 7 ​kbar followed by deformation during the retrograde phase at 480–515 ​°C and 6–7 ​kbar. The new geochronology data place an upper bound on the evolution of metamorphism and deformation in the frontal-most part of the Himalaya, which lasted until 17.5 ​Ma, as indicated by previously published 40Ar/39Ar data. The P-T-time data from this part of the Himalaya, as well as that from more hinterland-ward portions of the orogen, outline a progressive, stepwise, commonly out-of-sequence evolution. Further data from along the orogen indicates that this evolution is not a local phenomenon, but instead characterizes the tectonics of this system as a whole.http://www.sciencedirect.com/science/article/pii/S167498712030181XHimalayaMetamorphismKinematicsLu–Hf GeochronologyNepal
spellingShingle Kyle P. Larson
Sudip Shrestha
Mathieu Soret
Matthijs Smit
The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
Geoscience Frontiers
Himalaya
Metamorphism
Kinematics
Lu–Hf Geochronology
Nepal
title The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
title_full The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
title_fullStr The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
title_full_unstemmed The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
title_short The P-T-t-D evolution of the Mahabharat, east-central Nepal: The out-of-sequence development of the Himalaya
title_sort p t t d evolution of the mahabharat east central nepal the out of sequence development of the himalaya
topic Himalaya
Metamorphism
Kinematics
Lu–Hf Geochronology
Nepal
url http://www.sciencedirect.com/science/article/pii/S167498712030181X
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