Synthesis of the tectonic and structural elements of the Bengal Basin and its surroundings
MS Hossain, MSH Khan, KR Chowdhury… - Tectonics and structural …, 2019 - Springer
Abstract The Bengal Basin is a collisional foreland basin in South Asia located at the
juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …
juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …
Late Pleistocene-Holocene development of the Tista megafan (West Bengal, India): 10Be cosmogenic and IRSL age constraints
R Abrahami, P Huyghe, P van Der Beek… - Quaternary Science …, 2018 - Elsevier
The Himalayan proximal foreland is characterized by Quaternary megafans, of which the
formational mechanisms remain debated. The Tista megafan spreads over more than …
formational mechanisms remain debated. The Tista megafan spreads over more than …
Postseismic Deformation Following the 2015 Mw7.8 Gorkha (Nepal) Earthquake: New GPS Data, Kinematic and Dynamic Models, and the Roles of Afterslip and …
J Liu‐Zeng, Z Zhang, C Rollins… - Journal of …, 2020 - Wiley Online Library
Abstract We report Global Positioning System (GPS) measurements of postseismic
deformation following the 2015 Mw7. 8 Gorkha (Nepal) earthquake, including previously …
deformation following the 2015 Mw7. 8 Gorkha (Nepal) earthquake, including previously …
[HTML][HTML] Evaluation of ground motion parameters and seismic response of reinforced concrete buildings from the Mw 6.9, 2011 Sikkim earthquake
The continuous collision of the Eurasian plate and the Indian plate has resulted in several
earthquakes in the Himalayan region. The 6.9 Mw 2011 Sikkim earthquake, which caused …
earthquakes in the Himalayan region. The 6.9 Mw 2011 Sikkim earthquake, which caused …
Stochastic finite-fault method controlled by the fault rupture process and its application to the Ms 7.0 Lushan Earthquake
H Zhou, Y Chang - Soil Dynamics and Earthquake Engineering, 2019 - Elsevier
Fast and precise estimation of strong ground motion is important for seismic hazard
responses and engineering purposes. Stochastic finite-fault methods are effective ground …
responses and engineering purposes. Stochastic finite-fault methods are effective ground …
[HTML][HTML] 基于NNSIM 随机有限断层法的7.0 级九寨沟地震强地面运动场重建
周红 - 地球物理学报, 2018 - html.rhhz.net
北京时间2017 年8 月8 日21 时19 分在四川阿坝州九寨沟县(北纬33.2, 东经103.8) 发生了7.0
级地震, 作者利用新提出的震源破裂过程控制的NNSIM 随机有限断层方法, 对震中约100 km …
级地震, 作者利用新提出的震源破裂过程控制的NNSIM 随机有限断层方法, 对震中约100 km …
Assessment of maximum earthquake potential of the Kopili fault zone in northeast India and strong ground motion simulation
Maximum magnitude (MM) earthquake in the Kopili fault zone of North-East India has been
assessed using different approaches, which are primarily dependent on various parameters …
assessed using different approaches, which are primarily dependent on various parameters …
Evaluating the seismic hazard to Sikkim region of Himalaya using simulated accelerograms
R Yadav, D Kumar - Journal of Earth System Science, 2022 - Springer
Abstract The 2011 Sikkim earthquake (M 6.9) of the Himalaya has shown that a moderate
size earthquake may also cause severe damage to the region. Simulated accelerograms …
size earthquake may also cause severe damage to the region. Simulated accelerograms …
Rupture of the Indian slab in the 2011 Mw 6.9 Sikkim Himalaya earthquake and its tectonic implications
Unlike the other Himalayan plate boundary segments, the eastern Nepal to Bhutan
Himalayan region is not known to have generated prominent shallow thrust faulting …
Himalayan region is not known to have generated prominent shallow thrust faulting …
[PDF][PDF] Study of fault plane solutions and stress drop using local broadband network data: the 2011 Sikkim Himalaya earthquake of Mw 6.9 and its aftershocks
Fault plane solutions of the September 18, 2011 Sikkim Himalaya earthquake of Mw 6.9 and
its four aftershocks (Mw> 4.0) are studied by waveform inversion using the local broadband …
its four aftershocks (Mw> 4.0) are studied by waveform inversion using the local broadband …