Strong ground motion from the November 12, 2017, M 7.3 Kermanshah earthquake in western Iran
A Babaie Mahani, J Kazemian - Journal of Seismology, 2018 - Springer
In this paper, we analyzed the strong ground motion from the November 12, 2017,
Kermanshah earthquake in western Iran with moment magnitude (M) of 7.3. Nonlinear and …
Kermanshah earthquake in western Iran with moment magnitude (M) of 7.3. Nonlinear and …
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches
AK Pandey, P Chingtham, PNS Roy - Geomatics, Natural Hazards …, 2017 - Taylor & Francis
Regular seismic hazard assessment requires essentially an updated and refined
homogenous earthquake catalogue for the study region. Here, we have compiled the …
homogenous earthquake catalogue for the study region. Here, we have compiled the …
Local earthquake monitoring with a low-cost seismic network: a case study in Nepal
Seismic monitoring matters both for research and for populations living in areas of seismic
hazard; however, it comes with a cost that is not fully affordable for developing countries …
hazard; however, it comes with a cost that is not fully affordable for developing countries …
Earthquakes unveil the global-scale fractality of the lithosphere
The relationship between the magnitude of earthquakes and their spatial and temporal
distribution has been observed to exhibit a scale invariance hypothesised to originate from …
distribution has been observed to exhibit a scale invariance hypothesised to originate from …
Active Fault zones of the 2006 Yogyakarta earthquake inferred from tilt derivative analysis of gravity anomalies
L Handayani - RISET Geologi dan Pertambangan, 2019 - jrisetgeotam.brin.go.id
Abstract The 2006 Yogyakarta Earthquake had caused a disaster in Bantul area. Several
institutions had reported different results for the epicenter location. However, aftershocks …
institutions had reported different results for the epicenter location. However, aftershocks …
Analysis of the b, p values, and the fractal dimension of aftershocks sequences following two major earthquakes in central Himalaya
On April 25 of 2015, earthquake of 7.6 ML struck the central Himalayan region having
epicenter at Barpak village in the Gorkha district of Nepal. The event was followed by 7.0 ML …
epicenter at Barpak village in the Gorkha district of Nepal. The event was followed by 7.0 ML …
[HTML][HTML] Gorkha earthquake (MW7. 8) and aftershock sequence: A fractal approach
Abstract On April 25, 2015, Nepal was struck by the MW 7.8 Gorkha earthquake followed by
an intense aftershock sequence. It was one of the most destructive earthquakes in the …
an intense aftershock sequence. It was one of the most destructive earthquakes in the …
[PDF][PDF] Statistics of the earthquakes in the central Himalaya and its vicinity in last 56 years, with an emphasis in the 25 April 2015 Gorkha, Nepal earthquake
To understand the variation of stress levels in the region 80◦ E–89◦ E and 26◦ N–31◦ N, the
statistical analysis of earthquake frequency-magnitude distribution and spatio-temporal …
statistical analysis of earthquake frequency-magnitude distribution and spatio-temporal …
[HTML][HTML] Characteristics of earthquake swarm activity observed in the Palghar region of Indian Peninsula from January 2019 to October 2020
The present study emphasizes the seismic characteristics of earthquake swarm activity of
the Palghar region that occurred in the hard strata of Deccan traps of the Indian peninsula …
the Palghar region that occurred in the hard strata of Deccan traps of the Indian peninsula …
[HTML][HTML] On the spatio-temporal variation in b-value after 25 April 2015 Gorkha, Nepal earthquake
In the present study, the spatial-temporal distribution of b-value along the five faults area (the
Judi fault, Thaple fault, Kathmandu fault, Motihari-GauriShanker fault, and Motihari-Everest …
Judi fault, Thaple fault, Kathmandu fault, Motihari-GauriShanker fault, and Motihari-Everest …