Rupture of the Sunda megathrust on 26 December 2004 produced broad regions of uplift
and subsidence. We define the pivot line separating these regions as a first step in defining …

Abstract The Indian Ocean earthquake of 26 December 2004 led to significant ground
deformation in the Andaman and Nicobar region, accounting for∼ 800 km of the rupture …

Plate motion in the Indo‐Burmese Arc‐Andaman‐Sumatra region of Burma plate is poorly
resolved. This is mainly due to lack of relevant data and complex tectonics of the region. We …

The Andaman arc in the northeastern Indian Ocean defines nearly 1100 km long active plate
margin between the India and Burma plates where an oblique Benioff zone develops down …

Two field campaigns (March 2005 and March 2006) for measurements of biological
indicators and eyewitness accounts confirm that large coseismic and postseismic surface …

Abstract The December 2004 Indian Ocean Tsunami (IOT) had a major impact on the
geomorphology and sedimentology of the east coast of India. Estimation of the magnitude of …

Continued structural descent of the Indian lithosphere below the Sunda-Andaman trench
produced several destructive large to great earthquakes in the region of Andaman and …

The inter-specific resilience among mangrove species to sea level rise (SLR) is a key to
design conservation strategies for this economically important ecosystem that is among the …

Paleoseismic investigations have been carried out across an~ 10-m-high scarp along the
Carbyn thrust fault, that marks the structural contact between the overriding Ophiolite suite of …

The comparison of tiltmeter and strainmeter data in the periods of the strongest earthquakes
with tropical cyclone activities in the World Ocean during January–April 2014 is made. Main …