Add to ORKGThe Departement of Mines and Geology has been monitoring the seismicity of the Central Himalayas of Nepal since 1985. Intense microseismicity and frequent medium‐size earthquakes (mL<4) tend to cluster beneath the topographic front of the Higher Himalaya. This 10–20km deep seismicity also correlates with a zone of localized uplift that has been evidenced from geodetic data. Both microseismic and geodetic data indicate strain accumulation on a mid‐crustal ramp that had been previously inferred from geological and geophysical evidence. This ramp connects a flat decollement under the Lesser and Sub‐Himalaya with a deeper decollement under the Higher Himalaya, and probably acts as a geometric asperity where strain and stress build up during the...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
The mid-crustal ramp on the Main Himalayan Thrust (MHT) in the Lesser Himalaya Sequence (LHS) is the...
The Departement of Mines and Geology has been monitoring the seismicity of the Central Himalayas of ...
The seismic cycle on a major fault involves long periods of elastic strain and stress accumulation, ...
The National Seismological Network of Nepal consists of 17 short period seismic stations operated si...
Estimates of interseismic ground elevation change rates from Nepal Himalaya based on repeat levellin...
International audienceSUMMARY Unravelling relations between lateral variations of mid-crustal seismi...
A host of information is now available regarding the geological and thermal structure as well as def...
The Himalayan mountain range has been the locus of some of the largest continental earthquakes, incl...
The velocity of interseismic convergence through the Nepal Himalaya - essential parameter in the stu...
Underthrusting of the Indian lithosphere beneath the Himalayas occurs during the Quaternary period a...
The Main Himalayan Thrust (MHT) is the cardinal fault (décollement) that accommodates most of the re...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
The mid-crustal ramp on the Main Himalayan Thrust (MHT) in the Lesser Himalaya Sequence (LHS) is the...
The Departement of Mines and Geology has been monitoring the seismicity of the Central Himalayas of ...
The seismic cycle on a major fault involves long periods of elastic strain and stress accumulation, ...
The National Seismological Network of Nepal consists of 17 short period seismic stations operated si...
Estimates of interseismic ground elevation change rates from Nepal Himalaya based on repeat levellin...
International audienceSUMMARY Unravelling relations between lateral variations of mid-crustal seismi...
A host of information is now available regarding the geological and thermal structure as well as def...
The Himalayan mountain range has been the locus of some of the largest continental earthquakes, incl...
The velocity of interseismic convergence through the Nepal Himalaya - essential parameter in the stu...
Underthrusting of the Indian lithosphere beneath the Himalayas occurs during the Quaternary period a...
The Main Himalayan Thrust (MHT) is the cardinal fault (décollement) that accommodates most of the re...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustal...
The mid-crustal ramp on the Main Himalayan Thrust (MHT) in the Lesser Himalaya Sequence (LHS) is the...