Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2359-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-2359-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A 2600-year-long paleoseismic record for the Himalayan Main Frontal Thrust (western Bhutan)
Romain Le Roux-Mallouf
CORRESPONDING AUTHOR
Geolithe, Research and Development Department, Rue des Becasses, 38920, Crolles, France
Matthieu Ferry
Géosciences Montpellier, CNRS, UMR5243, Université de Montpellier, Place E. Bataillon, 34095 Montpellier, France
Rodolphe Cattin
Géosciences Montpellier, CNRS, UMR5243, Université de Montpellier, Place E. Bataillon, 34095 Montpellier, France
Jean-François Ritz
Géosciences Montpellier, CNRS, UMR5243, Université de Montpellier, Place E. Bataillon, 34095 Montpellier, France
Dowchu Drukpa
Géosciences Montpellier, CNRS, UMR5243, Université de Montpellier, Place E. Bataillon, 34095 Montpellier, France
Seismology and Geophysics Division, Department of Geology and Mines, P.O. Box 173, 9 Thimphu, Bhutan
Phuntsho Pelgay
Seismology and Geophysics Division, Department of Geology and Mines, P.O. Box 173, 9 Thimphu, Bhutan
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Cited
14 citations as recorded by crossref.
- Tomographic Image of Shear Wave Structure of NE India Based on Analysis of Rayleigh Wave Data A. Kumar et al. 10.3389/feart.2021.680361
- Surface rupture and landscape response in the middle of the great Mw 8.3 1934 earthquake mesoseismal area: Khutti Khola site M. Riesner et al. 10.1038/s41598-023-30697-7
- An embryonic fold and thrust belt south of the Himalayan morphological front: Examples from the Central Nepal and Darjeeling piedmonts J. Mugnier et al. 10.1016/j.earscirev.2022.104061
- Soft sediment deformation structures from the Brahmaputra Basin: A window to the eastern Himalayan paleoseismicity and tectonics A. Bhadran et al. 10.1016/j.jseaes.2023.105894
- Deformed alluvial terraces record an excess of slip over the last few centuries on the Himalayan Topographic Frontal Thrust of central Bhutan M. Gautier et al. 10.1038/s43247-024-01759-z
- Morphotectonic Evolution of an Alluvial Fan: Results of a Joint Analog and Numerical Modeling Approach C. Garcia-Estève et al. 10.3390/geosciences11100412
- Topographic disequilibrium, landscape dynamics and active tectonics: an example from the Bhutan Himalaya M. Simoes et al. 10.5194/esurf-9-895-2021
- Orogenic Segmentation and Its Role in Himalayan Mountain Building M. Hubbard et al. 10.3389/feart.2021.641666
- Himalayan Seismic Belt, Seismic Gaps and Related Issues H. Gupta 10.1007/s12594-023-2450-6
- Joint inversion of ground gravity data and satellite gravity gradients between Nepal and Bhutan: New insights on structural and seismic segmentation of the Himalayan arc R. Cattin et al. 10.1016/j.pce.2021.103002
- Paleoseismological evidence for segmentation of the Main Himalayan Thrust in the Darjeeling-Sikkim Himalaya A. Brice et al. 10.1038/s41598-024-63539-1
- Paleoseismological Findings at a New Trench Indicate the 1714 M8.1 Earthquake Ruptured the Main Frontal Thrust Over all the Bhutan Himalaya Y. Zhao et al. 10.3389/feart.2021.689457
- Damaging earthquakes of the Eastern Indian subcontinent and seismic hazard potential: insights from palaeoseismology A. Brice et al. 10.1080/00206814.2024.2341240
- Seismic hazard and risk in Bhutan V. Stevens et al. 10.1007/s11069-020-04275-3
13 citations as recorded by crossref.
- Tomographic Image of Shear Wave Structure of NE India Based on Analysis of Rayleigh Wave Data A. Kumar et al. 10.3389/feart.2021.680361
- Surface rupture and landscape response in the middle of the great Mw 8.3 1934 earthquake mesoseismal area: Khutti Khola site M. Riesner et al. 10.1038/s41598-023-30697-7
- An embryonic fold and thrust belt south of the Himalayan morphological front: Examples from the Central Nepal and Darjeeling piedmonts J. Mugnier et al. 10.1016/j.earscirev.2022.104061
- Soft sediment deformation structures from the Brahmaputra Basin: A window to the eastern Himalayan paleoseismicity and tectonics A. Bhadran et al. 10.1016/j.jseaes.2023.105894
- Deformed alluvial terraces record an excess of slip over the last few centuries on the Himalayan Topographic Frontal Thrust of central Bhutan M. Gautier et al. 10.1038/s43247-024-01759-z
- Morphotectonic Evolution of an Alluvial Fan: Results of a Joint Analog and Numerical Modeling Approach C. Garcia-Estève et al. 10.3390/geosciences11100412
- Topographic disequilibrium, landscape dynamics and active tectonics: an example from the Bhutan Himalaya M. Simoes et al. 10.5194/esurf-9-895-2021
- Orogenic Segmentation and Its Role in Himalayan Mountain Building M. Hubbard et al. 10.3389/feart.2021.641666
- Himalayan Seismic Belt, Seismic Gaps and Related Issues H. Gupta 10.1007/s12594-023-2450-6
- Joint inversion of ground gravity data and satellite gravity gradients between Nepal and Bhutan: New insights on structural and seismic segmentation of the Himalayan arc R. Cattin et al. 10.1016/j.pce.2021.103002
- Paleoseismological evidence for segmentation of the Main Himalayan Thrust in the Darjeeling-Sikkim Himalaya A. Brice et al. 10.1038/s41598-024-63539-1
- Paleoseismological Findings at a New Trench Indicate the 1714 M8.1 Earthquake Ruptured the Main Frontal Thrust Over all the Bhutan Himalaya Y. Zhao et al. 10.3389/feart.2021.689457
- Damaging earthquakes of the Eastern Indian subcontinent and seismic hazard potential: insights from palaeoseismology A. Brice et al. 10.1080/00206814.2024.2341240
1 citations as recorded by crossref.
Latest update: 14 Nov 2024
Short summary
The chronology of historical earthquakes (from historical documents and geological evidence) is still poorly constrained in the western Himalaya. We carried out a field investigation in SW Bhutan along the India–Bhutan border. Our analysis reveals that Bhutan has experienced at least five great earthquakes during the last 2600 years. Coseismic slip values along the Main Himalayan Thrust for most events reach at least 13 m and suggest that associated magnitudes are in the range of Mw 8.5–9.
The chronology of historical earthquakes (from historical documents and geological evidence) is...