Distribution of REEs and yttrium among major geochemical phases of marine Fe–Mn-oxides: Comparative study between hydrogenous and hydrothermal deposits

LS Prakash, D Ray, AL Paropkari, AV Mudholkar… - Chemical …, 2012 - Elsevier
Mineralogy and geochemistry of the ferromanganese oxides collected from two seamounts
in the Andaman Sea have been investigated with special reference to the solid phase …

The potential for giant tsunamigenic earthquakes in the northern Bay of Bengal

PR Cummins - Nature, 2007 - nature.com
Abstract The great Sumatra–Andaman earthquake and Indian Ocean tsunami of 2004 came
as a surprise to most of the earth science community. Although it is now widely recognized …

The northernmost part of the Great Sumatran Fault map and images derived from gravity anomaly

M Yanis, F Abdullah, N Zaini, N Ismail - Acta Geophysica, 2021 - Springer
Abstract The Great Sumatran Fault (GSF) activity is a severe threat to Banda Aceh
development as the capital city of Aceh Province, Indonesia. The earthquakes originating …

Influence of total organic carbon deposition on the inventory of gas hydrate in the Indian continental margins

JE Johnson, SC Phillips, ME Torres, E Piñero… - Marine and Petroleum …, 2014 - Elsevier
Total organic carbon (TOC) content of marine sediments represents residual carbon,
originally derived from terrestrial and marine sources, which has survived seafloor and …

Morphology and tectonics of the Andaman Forearc, northeastern Indian Ocean

JR Cochran - Geophysical Journal International, 2010 - academic.oup.com
Summary The Andaman Sea has developed as the result of highly oblique subduction at the
western Sunda Trench, leading to partitioning of convergence into trench-perpendicular and …

Continuity of great sumatran fault in the marine area revealed by 3D inversion of gravity data

Y Muhammad, A Faisal, A Yenny… - Jurnal Teknologi …, 2020 - journals.utm.my
The Great Sumatran Fault (GSF) is a 1900-km-long fault extending from Lampung,
Indonesia, to India's Andaman Islands. The fault location is not only on the land but also in …

Back‐arc extension in the Andaman Sea: Tectonic and magmatic processes imaged by high‐precision teleseismic double‐difference earthquake relocation

T Diehl, F Waldhauser, JR Cochran… - Journal of …, 2013 - Wiley Online Library
The geometry, kinematics, and mode of back‐arc extension along the Andaman Sea plate
boundary are refined using a new set of significantly improved hypocenters, global centroid …

The great Sumatra–Andaman earthquakes—imaging the boundary between the ruptures of the great 2004 and 2005 earthquakes

D Franke, M Schnabel, S Ladage, DR Tappin… - Earth and Planetary …, 2008 - Elsevier
Segmentation along convergent margins controls earthquake magnitude and location, but
the physical causes of segment boundaries, and their impact on earthquake rupture …

Burma plate motion

VK Gahalaut, K Gahalaut - Journal of Geophysical Research …, 2007 - Wiley Online Library
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 …

Stress change and effective friction coefficient along the Sumatra‐Andaman‐Sagaing fault system after the 26 December 2004 (Mw= 9.2) and the 28 March 2005 (Mw …

R Cattin, N Chamot‐Rooke, M Pubellier… - Geochemistry …, 2009 - Wiley Online Library
The 2004 Aceh and 2005 Nias events are the two greatest earthquakes of the past 40 years
with a total rupture of 1700 km long and a coseismic slip reaching up to 25 m. These two …