A review on out-of-sequence deformation in the Himalaya
S Mukherjee - Special Publications, 2015 - lyellcollection.org
Out-of-sequence deformation in the Himalaya has been caused mainly by thrusting. Out-of-
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
Orogenic segmentation and its role in Himalayan mountain building
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 …
reconfiguration of cratons throughout Earth history. Many of the mountain belts present today …
Extensional and compressional regime driven left-lateral shear in southwestern Anatolia (eastern Mediterranean): The Burdur-Fethiye Shear Zone
The tectonic framework of the eastern Mediterranean presented in this paper is based on an
active subduction and small underwater hills/mountains on the oceanic crust moving toward …
active subduction and small underwater hills/mountains on the oceanic crust moving toward …
Seismic zonation of Nepal using probabilistic seismic hazard analysis
Probabilistic seismic hazard of Nepal (PSHA) followed by seismic zonation is carried out for
enclosed polygon within 26.5° N–30.5° N latitude and 80° E–89° E longitude. Mixed type of …
enclosed polygon within 26.5° N–30.5° N latitude and 80° E–89° E longitude. Mixed type of …
Identifying seismicity pattern before major earthquakes in the Western Nepal and adjoining region (28.5°N to 31.0°N − 78°E to 82.96°E)
Earthquakes in the Himalayan region predominantly exhibit tectonic characteristics,
stemming from fault slippage caused by the ongoing collision between the Indian plate and …
stemming from fault slippage caused by the ongoing collision between the Indian plate and …
Geomorphological responses of rivers to active tectonics along the Siwalik Hills, Midwestern Nepalese Himalaya
Abstract The Nepalese Himalaya is well known for ongoing collisional tectonics, witnessed
by major historical and recent earthquakes. The Siwalik Hills in Midwestern Nepalese …
by major historical and recent earthquakes. The Siwalik Hills in Midwestern Nepalese …
Coseismic deformations of the 2015 MW 7.8 Gorkha earthquake and interseismic strain accumulation in the Himalayan tectonic belt and Tibetan plateau
Y Wu, Z Jiang, H Liang, L Chang, C Chen, S Zhu… - Tectonophysics, 2016 - Elsevier
The principal strain rate, derived from GPS velocities from the Tibetan Plateau and the India
Plate, shows that the Himalayan tectonic belt exhibits compression deformation in a NE–NS …
Plate, shows that the Himalayan tectonic belt exhibits compression deformation in a NE–NS …
Rupture processes of the 2015 Mw 7.9 Gorkha earthquake and its Mw 7.3 aftershock and their implications on the seismic risk
The rupture processes of the 2015 April 25 Gorkha earthquake and its strongest aftershock
occurred on May 12 in Nepal are investigated by joint inversion of seismological and …
occurred on May 12 in Nepal are investigated by joint inversion of seismological and …
Characteristic ground motions of the 25th April 2015 Nepal earthquake (Mw 7.9) and its implications for the structural design codes for the border areas of India to …
Abstract The 25th April 2015 Nepal Earthquake was found associated with a series of
aftershocks, and the mainshock rupture propagated predominantly towards SE direction …
aftershocks, and the mainshock rupture propagated predominantly towards SE direction …
Analysis of the b, p values, and the fractal dimension of aftershocks sequences following two major earthquakes in central Himalaya
On April 25 of 2015, earthquake of 7.6 ML struck the central Himalayan region having
epicenter at Barpak village in the Gorkha district of Nepal. The event was followed by 7.0 ML …
epicenter at Barpak village in the Gorkha district of Nepal. The event was followed by 7.0 ML …