Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Raphaele Moeremans"'
Autor:
Raphaele Moeremans, Satish C. Singh
Publikováno v:
Geological Society, London, Memoirs. 47:193-204
The Andaman–Nicobar subduction system is the northwestern segment of the Sunda subduction system, where the Indian Plate subducts beneath the Sunda Plate in a nearly arc-parallel direction. The entire segment ruptured during the 2004 great Andaman
Autor:
Raphaele Moeremans, Satish C. Singh
Publikováno v:
Tectonics. 34:1736-1750
The Andaman-Nicobar region is the northernmost segment of the Sumatra-Andaman subduction zone and marks the western boundary of the Andaman Sea, which is a complex active back-arc extensional basin. We present the interpretation of a new set of deep
Autor:
Satish C. Singh, Raphaele Moeremans
Publikováno v:
Geophysical Research Letters. 41:7143-7150
The NinetyEast Ridge (NER), one of the most enigmatic features in the Indian Ocean, is covered by thick Bengal Fan sediment north of 9°N. We present seismic reflection data on the eastern flank of the NER, at 10°N, that show the presence of 4–5 k
Publikováno v:
Earth and Planetary Science Letters. 386:75-85
Seven deep seismic reflection profiles cover the 3000 km-long subduction system from Andaman to Southern Sumatra, including zones that ruptured in 2004, 2007, and 2010. We find that (1) the frontal zone is characterized by a series of thrusts boundin
Publikováno v:
Journal of Geophysical Research: Solid Earth. 118:5208-5224
[1] The sliver strike-slip Great Sumatra Fault (GSF) traverses mainland Sumatra from the Sunda Strait in the southeast to Banda Aceh in the northwest, and defines the present day plate boundary between the Sunda Plate in the north and the Burmese Sli
Autor:
Ian Deighton, Haryadi Permana, M. Ma’ruf Mukti, Raphaele Moeremans, Satish C. Singh, Nugroho D. Hananto
Publikováno v:
Geochemistry, Geophysics, Geosystems. 13
[1] We present the interpretation of newly acquired high-quality industry-standard deep seismic reflection and swath bathymetry data to provide insight into the structural style and evolution of the Mentawai Fault Zone (MFZ). The MFZ lies along the b