Numerical fault simulation in Himalayas with 2 D finite element method

P(論文) The nature of the stress field in the Himalaya is examined by the 2D finite element method where linear elastic rheology and plain strain condition are assumed. The Mohr-Coulomb failure criterion has been adopted to analyze the relationship between stress distribution and fault formation.Two p...

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Main Authors: Howladar, M. Farhad, Hayashi, Daigoro
Language:English
Published: National Institute of Polar Research 2003
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3131/files/KJ00000044125.pdf
https://doi.org/10.15094/00003131
https://nipr.repo.nii.ac.jp/records/3131
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author Howladar, M. Farhad
Hayashi, Daigoro
author_facet Howladar, M. Farhad
Hayashi, Daigoro
author_sort Howladar, M. Farhad
collection National Institute of Polar Research Repository, Japan
description P(論文) The nature of the stress field in the Himalaya is examined by the 2D finite element method where linear elastic rheology and plain strain condition are assumed. The Mohr-Coulomb failure criterion has been adopted to analyze the relationship between stress distribution and fault formation.Two profile models are prepared and convergent displacement is imposed on them along the NE-SW horizontal direction.The convergent displacement and physical properties of the rock layer control the distribution,orientation,magnitude and intensity of the stress and fault development.According to the calculated stress pattern,thrust faults are expected to develop in the central Himalaya (model A).Normal and some thrust faults take place in the north-western Himalaya (model B).The results from our numerical experiment are in agreement with those from the seismicity and focal mechanism solution of earthquakes and also with those of M.M.Alam and D.Hayashi (Bull.Fac.Sci.Univ. Ryukyus, 73, 15, 2002) in the central Himalaya. departmental bulletin paper
genre Polar geoscience
genre_facet Polar geoscience
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003131
op_relation Polar geoscience
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243
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AA1130866X
https://nipr.repo.nii.ac.jp/record/3131/files/KJ00000044125.pdf
https://doi.org/10.15094/00003131
https://nipr.repo.nii.ac.jp/records/3131
publishDate 2003
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003131 2025-04-13T14:25:52+00:00 Numerical fault simulation in Himalayas with 2 D finite element method Howladar, M. Farhad Hayashi, Daigoro 2003-10 application/pdf https://nipr.repo.nii.ac.jp/record/3131/files/KJ00000044125.pdf https://doi.org/10.15094/00003131 https://nipr.repo.nii.ac.jp/records/3131 eng eng National Institute of Polar Research Polar geoscience 16 243 257 AA1130866X https://nipr.repo.nii.ac.jp/record/3131/files/KJ00000044125.pdf https://doi.org/10.15094/00003131 https://nipr.repo.nii.ac.jp/records/3131 numerical simulation fault Himalaya finite element method 2003 ftnipr https://doi.org/10.15094/00003131 2025-03-19T10:19:57Z P(論文) The nature of the stress field in the Himalaya is examined by the 2D finite element method where linear elastic rheology and plain strain condition are assumed. The Mohr-Coulomb failure criterion has been adopted to analyze the relationship between stress distribution and fault formation.Two profile models are prepared and convergent displacement is imposed on them along the NE-SW horizontal direction.The convergent displacement and physical properties of the rock layer control the distribution,orientation,magnitude and intensity of the stress and fault development.According to the calculated stress pattern,thrust faults are expected to develop in the central Himalaya (model A).Normal and some thrust faults take place in the north-western Himalaya (model B).The results from our numerical experiment are in agreement with those from the seismicity and focal mechanism solution of earthquakes and also with those of M.M.Alam and D.Hayashi (Bull.Fac.Sci.Univ. Ryukyus, 73, 15, 2002) in the central Himalaya. departmental bulletin paper Other/Unknown Material Polar geoscience National Institute of Polar Research Repository, Japan
spellingShingle numerical simulation
fault
Himalaya
finite element method
Howladar, M. Farhad
Hayashi, Daigoro
Numerical fault simulation in Himalayas with 2 D finite element method
title Numerical fault simulation in Himalayas with 2 D finite element method
title_full Numerical fault simulation in Himalayas with 2 D finite element method
title_fullStr Numerical fault simulation in Himalayas with 2 D finite element method
title_full_unstemmed Numerical fault simulation in Himalayas with 2 D finite element method
title_short Numerical fault simulation in Himalayas with 2 D finite element method
title_sort numerical fault simulation in himalayas with 2 d finite element method
topic numerical simulation
fault
Himalaya
finite element method
topic_facet numerical simulation
fault
Himalaya
finite element method
url https://nipr.repo.nii.ac.jp/record/3131/files/KJ00000044125.pdf
https://doi.org/10.15094/00003131
https://nipr.repo.nii.ac.jp/records/3131