Item request has been placed! ×
Item request cannot be made. ×
loading  Processing Request

Exhumation, crustal deformation, and thermal structure of the Nepal Himalaya derived from the inversion of thermochronological and thermobarometric data and modeling of the topography

Item request has been placed! ×
Item request cannot be made. ×
loading   Processing Request
  • معلومة اضافية
    • Contributors:
      Tectonics Observatory; California Institute of Technology (CALTECH); Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW); Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich); Department of Earth and Atmospheric Sciences Houston; University of Houston; DAM Île-de-France (DAM/DIF); Direction des Applications Militaires (DAM); Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA); Laboratoire de Sciences de la Terre (LST); École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL); Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS); Laboratoire de Géodynamique des Chaines Alpines (LGCA); Observatoire des Sciences de l'Univers de Grenoble (OSUG); Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS); Department of Geological Sciences Gainesville (UF|Geological); University of Florida Gainesville (UF); Institut für Geologie; Karl-Franzens-Universität Graz; Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE); Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
    • بيانات النشر:
      HAL CCSD
      American Geophysical Union
    • الموضوع:
      2010
    • Collection:
      Institut National de la Recherche Agronomique: ProdINRA
    • نبذة مختصرة :
      International audience ; Two end-member kinematic models of crustal shortening across the Himalaya are currently debated: one assumes localized thrusting along a single major thrust fault, the Main Himalayan Thrust (MHT) with nonuniform underplating due to duplexing, and the other advocates for out-of-sequence (OOS) thrusting in addition to thrusting along the MHT and underplating. We assess these two models based on the modeling of thermochronological, thermometric, and thermobarometric data from the central Nepal Himalaya. We complement a data set compiled from the literature with 114 40Ar/39Ar, 10 apatite fission track, and 5 zircon (U-Th)/He thermochronological data. The data are predicted using a thermokinematic model (PECUBE), and the model parameters are constrained using an inverse approach based on the Neighborhood Algorithm. The model parameters include geometric characteristics as well as overthrusting rates, radiogenic heat production in the High Himalayan Crystalline (HHC) sequence, the age of initiation of the duplex or of out-of-sequence thrusting. Both models can provide a satisfactory fit to the inverted data. However, the model with out-of-sequence thrusting implies an unrealistic convergence rate ≥30 mm yr‑1. The out-of-sequence thrust model can be adjusted to fit the convergence rate and the thermochronological data if the Main Central Thrust zone is assigned a constant geometry and a dip angle of about 30° and a slip rate of <1 mm yr‑1. In the duplex model, the 20 mm yr‑1 convergence rate is partitioned between an overthrusting rate of 5.8 ± 1.4 mm yr‑1 and an underthrusting rate of 14.2 ± 1.8 mm yr‑1. Modern rock uplift rates are estimated to increase from about 0.9 ± 0.31 mm yr‑1 in the Lesser Himalaya to 3.0 ± 0.9 mm yr‑1 at the front of the high range, 86 ± 13 km from the Main Frontal Thrust. The effective friction coefficient is estimated to be 0.07 or smaller, and the radiogenic heat production of HHC units is estimated to be 2.2 ± 0.1 μW m‑3. The midcrustal duplex initiated at 9.8 ...
    • Relation:
      insu-00549759; https://insu.hal.science/insu-00549759; https://insu.hal.science/insu-00549759/document; https://insu.hal.science/insu-00549759/file/2008JB006126.pdf; BIBCODE: 2010JGRB.11506407H
    • الرقم المعرف:
      10.1029/2008JB006126
    • الدخول الالكتروني :
      https://insu.hal.science/insu-00549759
      https://insu.hal.science/insu-00549759/document
      https://insu.hal.science/insu-00549759/file/2008JB006126.pdf
      https://doi.org/10.1029/2008JB006126
    • Rights:
      info:eu-repo/semantics/OpenAccess
    • الرقم المعرف:
      edsbas.32C828F6