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Colledge, Martin, Chanard, Kristel, Duverger, Clara, Schubnel, Alexandre, Adhikari, Lok Bijaya, and Bollinger, Laurent, 2025. Annual variations in Nepalese seismicity: b-values and seismicity rates. Geophysical Journal International, .
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025GeoJI.tmp..271C,
author = {{Colledge}, Martin and {Chanard}, Kristel and {Duverger}, Clara and {Schubnel}, Alexandre and {Adhikari}, Lok Bijaya and {Bollinger}, Laurent},
title = "{Annual variations in Nepalese seismicity: b-values and seismicity rates}",
journal = {Geophysical Journal International},
year = 2025,
month = jul,
abstract = "{Seasonal variations in Nepalese seismicity have been reported with
varying degrees of confidence. We re-investigate these claims by
analysing 20 years of Nepalese seismicity before the 2015 Gorkha
earthquake, as detected by the Nepalese national network, and
focusing on earthquakes located along the eastern and central
sections of the Nepalese Main Himalayan Thrust. Using several
declustering techniques, we find no statistically robust
evidence of seasonal seismicity in the studied record,
regardless of magnitude threshold above completeness. This
suggests that previously reported seasonality may be restricted
to the western section of the Nepalese orogeny, may be an
artefact, or may indicate that nucleation times of earthquakes
are longer than the year. We also investigate potential annual
variations in the Gutenberg-Richter b-value, given its recent
observed modulation by transient stressing. Additionally, we use
large-scale mass redistribution estimated from the monthly
gravity field retrieved from the Gravity Recovery And Climate
Experiment and Follow-On (GRACE/-FO) missions, to resolve stress
variations at depth induced by transient surface loads. We find
that the mean annual b-value peaks when seasonal Coulomb stress
rates reach their minimum value at the height of the summer
rainy season. When considering the combined effect of tectonic
and seasonal loading, this corresponds to a recurring period of
stress reversal, when Coulomb stress momentarily decreases. This
suggests that periodic clamping of the Main Himalayan Thrust
reduces the likelihood of earthquakes growing to larger
magnitudes in accordance with hierarchical rupture models. The
susceptibility of b-value to stress variations of roughly 0.1
points.kPa$^{-1}$ is consistent with recent estimates of b-value
sensitivity to transient loading, although it remains high when
compared to the stress-dependency associated with both static
differential stress, and with long-term evolution during the
seismic cycle. This discrepancy points to the large impact of
stress transients on the dynamics of seismic rupture.}",
doi = {10.1093/gji/ggaf259},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025GeoJI.tmp..271C},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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