The earthquake of 21 May 2014 (Mw 6.0) in the northern Bay of Bengal (BOB) highlights the importance of studies on intraplate earthquakes in the oceanic regime for understanding the stress state of the oceanic lithosphere. The epicenter of the earthquake is located at a water depth of 2.5 km where the sediment thickness is nearly 12 km, and it occurs at a depth of similar to 50 km within the upper mantle. Its location on the seismotectonic map of the region shows that the epicenter is far from the seismically active zone of the Burmese Arc in the east and low-to-moderately active seismic region of the east coast of India in the west. The fault plane solution of this earthquake indicates that it was a strike-slip event with a right-lateral s...
The Andaman-Nicobar Islands in the Bay of Bengal lies in a zone where the Indian plate subducts bene...
The 2016 M-w 6.7 Imphal earthquake is one of the largest and instrumentally well-recorded seismic ev...
Abstract. Throughout the world, the tsunami generation po-tential of some large under-sea earthquake...
Oceanic intraplate earthquakes are known to occur either on active ridge-transform structures or by ...
Oceanic intraplate earthquakes are known to occur either on active ridge-transform structures or by ...
International audienceNew multi-channel seismic data were acquired in the northern part of the Bay o...
International audienceNew multi-channel seismic data were acquired in the northern part of the Bay o...
The similar to 1300-km-long rupture zone of the 2004 Andaman-Sumatra megathrust earthquake continues...
New multi-channel seismic data were acquired in the northern part of the Bay of Bengal and at the no...
The 1300-km rupture of the 2004 interplate earthquake terminated at around 15 degrees N, in the nort...
The 11 April 2012 earthquakes (M-w 8.6 and M-w 8.2) were sourced within the Northern Wharton Basin i...
The 1300-km rupture of the 2004 interplate earthquake terminated at around 15 degrees N, in the nort...
The 11 April 2012 earthquakes (M-w 8.6 and M-w 8.2) were sourced within the Northern Wharton Basin i...
Earthquakes in the Indo-Burmese wedge occur due to India-Sunda plate motion. These earthquakes gener...
beneath the Indian Ocean. Both earthquakes were predominantly left-lateral strike-slip on vertical N...
The Andaman-Nicobar Islands in the Bay of Bengal lies in a zone where the Indian plate subducts bene...
The 2016 M-w 6.7 Imphal earthquake is one of the largest and instrumentally well-recorded seismic ev...
Abstract. Throughout the world, the tsunami generation po-tential of some large under-sea earthquake...
Oceanic intraplate earthquakes are known to occur either on active ridge-transform structures or by ...
Oceanic intraplate earthquakes are known to occur either on active ridge-transform structures or by ...
International audienceNew multi-channel seismic data were acquired in the northern part of the Bay o...
International audienceNew multi-channel seismic data were acquired in the northern part of the Bay o...
The similar to 1300-km-long rupture zone of the 2004 Andaman-Sumatra megathrust earthquake continues...
New multi-channel seismic data were acquired in the northern part of the Bay of Bengal and at the no...
The 1300-km rupture of the 2004 interplate earthquake terminated at around 15 degrees N, in the nort...
The 11 April 2012 earthquakes (M-w 8.6 and M-w 8.2) were sourced within the Northern Wharton Basin i...
The 1300-km rupture of the 2004 interplate earthquake terminated at around 15 degrees N, in the nort...
The 11 April 2012 earthquakes (M-w 8.6 and M-w 8.2) were sourced within the Northern Wharton Basin i...
Earthquakes in the Indo-Burmese wedge occur due to India-Sunda plate motion. These earthquakes gener...
beneath the Indian Ocean. Both earthquakes were predominantly left-lateral strike-slip on vertical N...
The Andaman-Nicobar Islands in the Bay of Bengal lies in a zone where the Indian plate subducts bene...
The 2016 M-w 6.7 Imphal earthquake is one of the largest and instrumentally well-recorded seismic ev...
Abstract. Throughout the world, the tsunami generation po-tential of some large under-sea earthquake...