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A statistical approach to relationships between fluid emissions and faults: The Sea of Marmara case ArchiMer
Henry, P.; Grall, Celine; Kende, J.; Viseur, S.; Ozeren, M. S.; Sengor, A. M. C.; Dupre, Stephanie; Scalabrin, Carla; Geli, Louis.
The Sea of Marmara is traversed by the North Anatolian Fault system and also presents abundant emission sites of methane gas into the water column. In order to assess the spatial relationship between gas emissions and active faults, the distribution of distances between gas emission sites and the nearest fault is calculated and compared with the distribution of distances between a uniform random distribution of points (Poisson process representing the null hypothesis of an absence of relationship between gas emissions and faults) and the nearest fault. Interestingly, the distance distribution for the Poisson process is nearly exponential, indicating that the fault map does not have a characteristic scale other than that representing the intensity of the...
Tipo: Text Palavras-chave: Cold seeps; Gas emissions; Transform plate boundary; Strike-slip fault; Damage zone.
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00441/55252/56739.pdf
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New insights on the offshore extension of the Great Sumatran fault, NW Sumatra, from marine geophysical studies ArchiMer
Ghosal, D.; Singh, S.c.; Chauhan, A. P. S.; Hananto, N. D..
Over the last 20 years, the Great Sumatran Fault (GSF) has been studied on land, but we have very little information about its offshore extension NW of Sumatra and its link with the West Andaman Fault to the north. The problem is further complicated by its vicinity to the volcanic arc. Here we present detailed analyses of the offshore extension of the GSF based on recently acquired high-resolution bathymetry, multichannel seismic reflection data and some old single channel seismic reflection data. Our findings demonstrate that the branches of the GSF near Banda Aceh proceed further northwestward producing two 15-20 km wide adjacent basins. The southwestern transpressional Breueh basin is 1-2 km deep and has a flower structure with a push-up ridge in the...
Tipo: Text Palavras-chave: Great Sumatra Fault; Back-arc spreading; Pull-apart basin; Strike-slip fault; Volcanic arc.
Ano: 2012 URL: https://archimer.ifremer.fr/doc/00265/37600/36899.pdf
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