International audiencehe Himalayan orogen has produced three thrust earthquakes with moment magnitude (Mw) 7.8 to 8.5 during the past century, yet no surface ruptures associated with these great earthquakes have been documented. Here, we present paleoseismic evidence from east central Nepal that, since ~700 A.D., a single earthquake ruptured the Frontal Thrust fault at ~1100 A.D., with a surface displacement of ~17 (+5/–3) meters and a lateral extent and size that could have exceeded 240 kilometers and ~Mw 8.8, respectively. Ruptures associated with Mw <8.2 events would contribute to the frontal Himalayas folding but would stop before reaching the surface. These findings could require substantial modifications to current regional seismic ha...
International audienceThe return times of large Himalayan earthquakes are poorly constrained. Despit...
Abstract The Himalaya is one of the most seismically active regions of the world. The occurrence of ...
International audienceAccording to paleoseismological studies, the last earthquake that ruptured the...
International audiencehe Himalayan orogen has produced three thrust earthquakes with moment magnitud...
The Himalaya has experienced three great earthquakes during the last century1934 Nepal-Bihar, 1950 U...
International audienceThe seismic behavior of the Himalayan arc between central Nepal and Arunachal ...
The 1714 Bhutan earthquake was one of the largest in the Himalaya in the last millennium. We show th...
The foothills of the Himalaya bordered by the Main Frontal Thrust (MFT) continue to be a locus of pa...
Although the Main Himalayan Frontal Thrust (MHT/MFT), largest and fastest slipping continental megat...
Toward understanding the relationship between strain accumulation and strain release in the context ...
The similar to 2500 km long Himalayan arc has experienced three large to great earthquakes of M-w 7....
In 1255, 1344, and 1408 AD, then again in 1833, 1934, and 2015, large earthquakes, devastated Kathma...
International audienceThe return times of large Himalayan earthquakes are poorly constrained. Despit...
Abstract The Himalaya is one of the most seismically active regions of the world. The occurrence of ...
International audienceAccording to paleoseismological studies, the last earthquake that ruptured the...
International audiencehe Himalayan orogen has produced three thrust earthquakes with moment magnitud...
The Himalaya has experienced three great earthquakes during the last century1934 Nepal-Bihar, 1950 U...
International audienceThe seismic behavior of the Himalayan arc between central Nepal and Arunachal ...
The 1714 Bhutan earthquake was one of the largest in the Himalaya in the last millennium. We show th...
The foothills of the Himalaya bordered by the Main Frontal Thrust (MFT) continue to be a locus of pa...
Although the Main Himalayan Frontal Thrust (MHT/MFT), largest and fastest slipping continental megat...
Toward understanding the relationship between strain accumulation and strain release in the context ...
The similar to 2500 km long Himalayan arc has experienced three large to great earthquakes of M-w 7....
In 1255, 1344, and 1408 AD, then again in 1833, 1934, and 2015, large earthquakes, devastated Kathma...
International audienceThe return times of large Himalayan earthquakes are poorly constrained. Despit...
Abstract The Himalaya is one of the most seismically active regions of the world. The occurrence of ...
International audienceAccording to paleoseismological studies, the last earthquake that ruptured the...