Back-projection imaging of earthquakes
E Kiser, M Ishii - Annual Review of Earth and Planetary Sciences, 2017 - annualreviews.org
Back-projection analysis of earthquakes is a type of array processing that images the source
of seismic waves coherently recorded at stations throughout the seismic network. The …
of seismic waves coherently recorded at stations throughout the seismic network. The …
Seismotectonic perspectives on the Himalayan arc and contiguous areas: Inferences from past and recent earthquakes
K Rajendran, RM Parameswaran, CP Rajendran - Earth-Science Reviews, 2017 - Elsevier
Spread over countries including Pakistan, India, Nepal, Bhutan, and China, the Himalayan
mountain chain, the most spectacular result of the Indo-Eurasian plate collision, is a locus of …
mountain chain, the most spectacular result of the Indo-Eurasian plate collision, is a locus of …
New empirical earthquake source‐scaling laws
KKS Thingbaijam, PM Mai… - Bulletin of the …, 2017 - pubs.geoscienceworld.org
We develop new empirical scaling laws for rupture width W, rupture length L, rupture
area A, and average slip D, based on a large database of rupture models. The database …
area A, and average slip D, based on a large database of rupture models. The database …
Rupture process of the Mw = 7.9 2015 Gorkha earthquake (Nepal): Insights into Himalayan megathrust segmentation
We investigate the rupture process of the 25 April 2015 Gorkha earthquake (Mw= 7.9) using
a kinematic joint inversion of teleseismic waves, strong motion data, high‐rate GPS, static …
a kinematic joint inversion of teleseismic waves, strong motion data, high‐rate GPS, static …
Strong ground motion in the Kathmandu Valley during the 2015 Gorkha, Nepal, earthquake
On 25 April 2015, a large earthquake of Mw 7.8 occurred along the Main Himalayan Thrust
fault in central Nepal. It was caused by a collision of the Indian Plate beneath the Eurasian …
fault in central Nepal. It was caused by a collision of the Indian Plate beneath the Eurasian …
The 2015 Gorkha earthquake: a large event illuminating the Main Himalayan Thrust fault
Z Duputel, J Vergne, L Rivera… - Geophysical …, 2016 - Wiley Online Library
The 2015 Gorkha earthquake sequence provides an outstanding opportunity to better
characterize the geometry of the Main Himalayan Thrust (MHT). To overcome limitations due …
characterize the geometry of the Main Himalayan Thrust (MHT). To overcome limitations due …
Coseismic and early postseismic deformation due to the 25 April 2015, Mw 7.8 Gorkha, Nepal, earthquake from InSAR and GPS measurements
Abstract Analysis of Interferometric Synthetic Aperture Radar (InSAR) and Global Positioning
System (GPS) data reveals coseismic and early postseismic (4–88 days) surface …
System (GPS) data reveals coseismic and early postseismic (4–88 days) surface …
Constraining central Himalayan (Nepal) fault geometry through integrated thermochronology and thermokinematic modeling
Constraining the subsurface structural geometry of the central Himalaya continues to prove
difficult, even after the 2015 Gorkha earthquake and the resulting insights into the trajectory …
difficult, even after the 2015 Gorkha earthquake and the resulting insights into the trajectory …
Improving back projection imaging with a novel physics‐based aftershock calibration approach: A case study of the 2015 Gorkha earthquake
Abstract The 2015 Mw 7.8 Nepal‐Gorkha earthquake with casualties of over 9000 people
was the most devastating disaster to strike Nepal since the 1934 Nepal‐Bihar earthquake …
was the most devastating disaster to strike Nepal since the 1934 Nepal‐Bihar earthquake …
Source characteristics of the 2015 MW 7.8 Gorkha (Nepal) earthquake and its MW 7.2 aftershock from space geodesy
Abstract On April 25, 2015, a destructive MW 7.8 earthquake struck the capital of Nepal,
Kathmandu, killing more than 8800 people and destroying numerous historical structures …
Kathmandu, killing more than 8800 people and destroying numerous historical structures …