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Cenozoic tectonic evolution of regional fault systems in the SE Tibetan Plateau
Abstract The SE Tibetan Plateau, tectonically situated in the eastern India-Eurasia oblique
convergence zone, has experienced multiple stages of deformation since the Cenozoic …
convergence zone, has experienced multiple stages of deformation since the Cenozoic …
Active tectonics and earthquake potential of the Myanmar region
This paper describes geomorphologic evidence for the principal neotectonic features of
Myanmar and its immediate surroundings. We combine this evidence with published …
Myanmar and its immediate surroundings. We combine this evidence with published …
The 2011 MW 6.8 Burma earthquake: fault constraints provided by multiple SAR techniques
We used two tracks of ALOS PALSAR images to investigate the focal mechanism and slip
distribution of the 2011 March 24, MW 6.8 Burma strike-slip earthquake. Three different SAR …
distribution of the 2011 March 24, MW 6.8 Burma strike-slip earthquake. Three different SAR …
[HTML][HTML] Southeastern margin of the Tibetan Plateau stopped expanding in the late Miocene
The birth and expansion of continental plateaus exert a strong control on our planet's climate
and the distribution and evolution of its biodiversity. It has been proposed that the Tibetan …
and the distribution and evolution of its biodiversity. It has been proposed that the Tibetan …
On the relationship between strain rate and seismicity in the India–Asia collision zone: implications for probabilistic seismic hazard
The increasing density of geodetic measurements makes it possible to map surface strain
rate in many zones of active tectonics with unprecedented spatial resolution. Here we show …
rate in many zones of active tectonics with unprecedented spatial resolution. Here we show …
New GNSS and geological data from the Indo‐Burman subduction zone indicate active convergence on both a locked megathrust and the Kabaw Fault
Abstract The Indo‐Burma subduction zone is a highly oblique subduction system where the
Indian plate is converging with the Eurasian plate. How strain is partitioned between the …
Indian plate is converging with the Eurasian plate. How strain is partitioned between the …
Active subduction and strain partitioning in western Myanmar revealed by a dense survey GNSS network
The active tectonics of the Myanmar (formerly Burma) microplate in central Myanmar are
caused by the oblique collision between the Sunda and Eurasia plates to the east and the …
caused by the oblique collision between the Sunda and Eurasia plates to the east and the …
A 3‐D shear wave velocity model for Myanmar region
Myanmar is located at the eastern margin of the ongoing Indo‐Eurasian collision system,
has experienced a complex tectonic history and is threatened by a high level of seismic …
has experienced a complex tectonic history and is threatened by a high level of seismic …
Active tectonics of Myanmar and the Andaman Sea
Burma (Myanmar) is situated along the obliquely colliding eastern margin of the Indian Plate
(Fig. 2.1). It connects the ongoing India–Asia collision along the Himalayan Range in the …
(Fig. 2.1). It connects the ongoing India–Asia collision along the Himalayan Range in the …
Tectonic landform and paleoseismic events of the easternmost Matano fault in Sulawesi, Indonesia
The 190-km-long Matano fault is a major left-lateral strike-slip fault in Sulawesi, Indonesia
that accommodates the rapid westward motion of the Pacific plate relative to the Australian …
that accommodates the rapid westward motion of the Pacific plate relative to the Australian …