P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its geological framework and initial growth were fundamentally the result of multiple, previous …
The continental collision process has made a large contribution to continental growth and reconfiguration of cratons throughout Earth history. Many of the mountain belts present today …
Abstract In 1255, 1344, and 1408 AD, then again in 1833, 1934, and 2015, large earthquakes, devastated Kathmandu. The 1255 and 1934 surface ruptures have been …
We analyze time series from continuously recording GPS stations in Nepal spanning the pre- and post-seismic period associated to the M w 7.8 Gorkha earthquake which ruptured the …
Abstract Rupture in the 2015 M7. 8 Gorkha earthquake nucleated at the downdip edge of the Main Himalayan Thrust (MHT) near the transition from interseismic locking to aseismic creep …
Abstract The Himalayan Main Frontal Thrust (MFT) currently accommodates approximately half, ie, 12–23 mm/yr, of the convergence between the Indian and Eurasian tectonic plates …
The 2015 Gorkha earthquake produced displacement on the lower half of a shallow decollement that extends 100 km south, and upward from beneath the High Himalaya and …
VL Stevens, SN Shrestha… - Bulletin of the …, 2018 - pubs.geoscienceworld.org
We carry out a new probabilistic seismic hazard analysis (PSHA) for Nepal. The 2015 M w 7.8 Gorkha, Nepal, earthquake (hereafter the Gorkha earthquake) highlights the seismic risk …
The importance of understanding earthquake sources in India and Nepal was underscored by the disastrous 2015 earthquakes of 25 April Gorkha (Mw 7.8) and 12 May Kodari (Mw 7.3 …