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Open AccessJournal ArticleDOI

The 2015 Gorkha Nepal Earthquake: Insights from Earthquake Damage Survey

TLDR
In this article, the authors reviewed the seismotectonic setting and regional seismicity in Nepal and analyzes available aftershock data and ground motion data to gain deeper understanding of the observed earthquake damage in Nepal.
Abstract
The 2015 Gorkha Nepal earthquake caused tremendous damage and loss. To gain valuable lessons from this tragic event, an earthquake damage investigation team was dispatched to Nepal from 1 May 2015 to 7 May 2015. A unique aspect of the earthquake damage investigation is that first-hand earthquake damage data were obtained 6 to 11 days after the mainshock. To gain deeper understanding of the observed earthquake damage in Nepal, the paper reviews the seismotectonic setting and regional seismicity in Nepal and analyzes available aftershock data and ground motion data. The earthquake damage observations indicate that the majority of the damaged buildings were stone/brick masonry structures with no seismic detailing, whereas the most of RC buildings were undamaged. This indicates that adequate structural design is the key to reduce the earthquake risk in Nepal. To share the gathered damage data widely, the collected damage data (geo-tagged photos and observation comments) are organized using Google Earth and the kmz file is made publicly available.

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Rupture process of the Mw = 7.9 2015 Gorkha earthquake (Nepal): Insights into Himalayan megathrust segmentation

TL;DR: In this article, the authors investigated the rupture process of the 25 April 2015 Gorkha earthquake using a kinematic joint inversion of teleseismic waves, strong motion data, high-rate GPS, static GPS, and synthetic aperture radar (SAR) data.
Journal ArticleDOI

A global slope unit-based method for the near real-time prediction of earthquake-induced landslides

TL;DR: In this article, a set of 25 earthquake-induced landslide-events are selected and categorized based on the similarity between causal factors to determine the most relevant training set to make a prediction for a given landslide-event.
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An updated method for estimating landslide-event magnitude

TL;DR: In this article, the authors used a much larger collection of earthquake-induced landslide (EQIL) inventories (n=45) than previous studies to show that size distributions are much more variable than previously assumed.
Journal ArticleDOI

Reconnaissance report on geotechnical and structural damage caused by the 2015 Gorkha Earthquake, Nepal

TL;DR: In this paper, a field survey was conducted in Kathmandu, Trishuli, Melamchi, Baluwa (epicentral area) and Pokhara from 1 to 6 May 2015.
References
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Journal ArticleDOI

Ground-motion prediction equations for the average horizontal component of PGA, PGV, and 5%-damped PSA at spectral periods between 0.01 s and 10.0 s

TL;DR: In this article, the authors derived ground motion prediction equations for average horizontal-component ground motions as a function of earthquake magnitude, distance from source to site, local average shear-wave velocity, and fault type.
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NGA-West2 Equations for Predicting PGA, PGV, and 5% Damped PSA for Shallow Crustal Earthquakes:

TL;DR: In this article, ground motion prediction equations for computing median and standard deviations of average horizontal component intensity measures (IMs) for shallow crustal earthquakes in active tectonic regions were provided.

Review Article Topographic Slope as a Proxy for Seismic Site Conditions and Amplification

TL;DR: In this paper, a technique to derive first-order site-condition maps from topographic data is described, where the average shear-velocity down to 30 m is correlated against topographic slope to develop two sets of parameters for deriving VS 30 : one for active tectonic regions where to-pographic relief is high, and one for stable shields where topography is sparse.
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Magnitude calibration of north Indian earthquakes

TL;DR: In this article, the size and location of northern Indian and southern Tibetan earthquakes during the last 200 years is evaluated. But the authors focus on assessing intensity of early and more recent earthquakes in a built environment and to the way in which isoseismals are drawn.
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