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...
Main Authors: | , |
---|---|
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 |
_version_ | 1829314255399157760 |
---|---|
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 |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00003131 |
institution | Open Polar |
language | English |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00003131 |
op_relation | 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 |
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 |