International audienceWe present the first recorded global positioning system (GPS) data from Myanmar measured at the northern tip of the Sagaing fault. This area is in a very complex geodynamic context, where rigid and semirigid plates interact. The 12 GPS sites measured in 2005 and 2008 in northern Myanmar show that the slip rate is 18 mm/yr and is localized along a single active narrow fault trace (<20 km wide). The same rate was previously demonstrated and remeasured, 500 km southward, in central Myanmar. Despite the geodynamic regional complexity induced by interaction between the Sunda and India plates, the Burma microplate, and the highly deformable eastern Himalayan syntaxis, the slip rate remains surprisingly constant along this fa...
Several models of plate boundary and convergence between the Indian and South China plate across the...
International audienceThe ∼1200 km long north-south oriented Sagaing fault (plate boundary fault bet...
The northeastern Tibetan Plateau and its surroundings are a tectonically complex region resulting fr...
International audienceWe present the first recorded global positioning system (GPS) data from Myanma...
The Sagaing Fault is a major tectonic structure between the Indian Plate and Sunda Plate. The fault ...
Characterizing the 700 km wide system of active faults on the Shan Plateau, southeast of the eastern...
International audienceUsing a regional GPS data set including ∼190 stations in Asia, from Nepal to e...
[1] Using a regional GPS data set including 190 stations in Asia, from Nepal to eastern Indonesia an...
The Rakhine (Arakan)‐Bangladesh megathrust, along which the Indian and Burma plates collide, is assu...
The motion between India and Sunda plates is accommodated along the Churachandpur Mao Fault (CMF) in...
Abstract. We present and interpret Global Positioning System (GPS) measurements of crustal motions f...
International audiencePrevious estimates of the geodetic and geologic slip rates of the 1500 km long...
Tectonics and earthquake occurrence processes of the two Himalayan syntaxes are complex. Their limit...
We investigate the seismically active and tectonically complex oblique subduction system in Myanmar,...
Observations of relative motion in a geodetic network in Ladakh, India, and across southern Tibet in...
Several models of plate boundary and convergence between the Indian and South China plate across the...
International audienceThe ∼1200 km long north-south oriented Sagaing fault (plate boundary fault bet...
The northeastern Tibetan Plateau and its surroundings are a tectonically complex region resulting fr...
International audienceWe present the first recorded global positioning system (GPS) data from Myanma...
The Sagaing Fault is a major tectonic structure between the Indian Plate and Sunda Plate. The fault ...
Characterizing the 700 km wide system of active faults on the Shan Plateau, southeast of the eastern...
International audienceUsing a regional GPS data set including ∼190 stations in Asia, from Nepal to e...
[1] Using a regional GPS data set including 190 stations in Asia, from Nepal to eastern Indonesia an...
The Rakhine (Arakan)‐Bangladesh megathrust, along which the Indian and Burma plates collide, is assu...
The motion between India and Sunda plates is accommodated along the Churachandpur Mao Fault (CMF) in...
Abstract. We present and interpret Global Positioning System (GPS) measurements of crustal motions f...
International audiencePrevious estimates of the geodetic and geologic slip rates of the 1500 km long...
Tectonics and earthquake occurrence processes of the two Himalayan syntaxes are complex. Their limit...
We investigate the seismically active and tectonically complex oblique subduction system in Myanmar,...
Observations of relative motion in a geodetic network in Ladakh, India, and across southern Tibet in...
Several models of plate boundary and convergence between the Indian and South China plate across the...
International audienceThe ∼1200 km long north-south oriented Sagaing fault (plate boundary fault bet...
The northeastern Tibetan Plateau and its surroundings are a tectonically complex region resulting fr...