Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust
Abstract
The interaction between seasonally-induced non-tectonic and tectonic deformation along the Himalayan plate boundary remains debated. Here, we propose that tectonic deformation along this plate boundary can be significantly influenced by the deformation induced by the non-tectonic hydrological loading cycles. We explore seasonal mass oscillations by continental water storage in Southeast Asia and Himalayan arc region using continuous Global Positioning System measurements and satellite data from the Gravity Recovery and Climate Experiment. We suggest that the substantially higher transient displacements above the base of the seismogenic zone indicate a role of changes in aseismic slip rate on the deep megathrust that may be controlled by seasonal hydrological loading. We invoke modulation of aseismic slip on the megathrust down-dip of the seismogenic zone due to a fault resonance process induced by the seasonal stress changes. This process modulates mid-crustal ramp associated micro-seismicity and influences the timing of Central Himalayan earthquakes.
- Authors:
-
- National Institute of Technology (NIT), Rourkela (India)
- National Centre for Seismology, New Delhi (India)
- Univ. of California, Berkeley, CA (United States)
- Univ. of South California, Los Angeles, CA (United States)
- Indian Inst. of Technology, Kanpur (India)
- CSIR-National Geophysical Research Inst., Hyderabad (India)
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1567134
- Grant/Contract Number:
- AC02-05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Nature Communications
- Additional Journal Information:
- Journal Volume: 9; Journal Issue: 1; Journal ID: ISSN 2041-1723
- Publisher:
- Nature Publishing Group
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Panda, Dibyashakti, Kundu, Bhaskar, Gahalaut, Vineet K., Bürgmann, Roland, Jha, Birendra, Asaithambi, Renuhaa, Yadav, Rajeev Kumar, Vissa, Naresh Krishna, and Bansal, Amit Kumar. Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust. United States: N. p., 2018.
Web. doi:10.1038/s41467-018-06371-2.
Panda, Dibyashakti, Kundu, Bhaskar, Gahalaut, Vineet K., Bürgmann, Roland, Jha, Birendra, Asaithambi, Renuhaa, Yadav, Rajeev Kumar, Vissa, Naresh Krishna, & Bansal, Amit Kumar. Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust. United States. https://doi.org/10.1038/s41467-018-06371-2
Panda, Dibyashakti, Kundu, Bhaskar, Gahalaut, Vineet K., Bürgmann, Roland, Jha, Birendra, Asaithambi, Renuhaa, Yadav, Rajeev Kumar, Vissa, Naresh Krishna, and Bansal, Amit Kumar. Mon .
"Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust". United States. https://doi.org/10.1038/s41467-018-06371-2. https://www.osti.gov/servlets/purl/1567134.
@article{osti_1567134,
title = {Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust},
author = {Panda, Dibyashakti and Kundu, Bhaskar and Gahalaut, Vineet K. and Bürgmann, Roland and Jha, Birendra and Asaithambi, Renuhaa and Yadav, Rajeev Kumar and Vissa, Naresh Krishna and Bansal, Amit Kumar},
abstractNote = {The interaction between seasonally-induced non-tectonic and tectonic deformation along the Himalayan plate boundary remains debated. Here, we propose that tectonic deformation along this plate boundary can be significantly influenced by the deformation induced by the non-tectonic hydrological loading cycles. We explore seasonal mass oscillations by continental water storage in Southeast Asia and Himalayan arc region using continuous Global Positioning System measurements and satellite data from the Gravity Recovery and Climate Experiment. We suggest that the substantially higher transient displacements above the base of the seismogenic zone indicate a role of changes in aseismic slip rate on the deep megathrust that may be controlled by seasonal hydrological loading. We invoke modulation of aseismic slip on the megathrust down-dip of the seismogenic zone due to a fault resonance process induced by the seasonal stress changes. This process modulates mid-crustal ramp associated micro-seismicity and influences the timing of Central Himalayan earthquakes.},
doi = {10.1038/s41467-018-06371-2},
journal = {Nature Communications},
number = 1,
volume = 9,
place = {United States},
year = {Mon Oct 08 00:00:00 EDT 2018},
month = {Mon Oct 08 00:00:00 EDT 2018}
}
Web of Science
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