High-resolution 3-D seismic data acquired in the Sea of Marmara on the Western High, along the northwestern branch of the North Anatolian Fault (also known as the Main Marmara Fault), shed new light on the evolution of the deformation over the last 500-600 ka. Sedimentary sequences in ponded basins are correlated with glacioeustatic cycles and transitions between marine and low sea/lake environments in the Sea of Marmara. In the 3 x 11 km(2) of the 3-D seismic survey, deformation over the last 405-490 ka is localized along the main fault branch and north of it, where N130 degrees-N140 degrees trending normal faults and N40 degrees-N50 degrees folding accommodated strike-slip deformation associated with active argillokinesis. There is some e...
Since the 1999 Izmit-Kocaeli earthquake, the Main Marmara Fault (MMF) of the North Anatolian Fault s...
The North Anatolian Fault (NAF) zone is 1500 km long, extending almost up to the Greek mainland in t...
International audienceThe North Anatolian Fault (NAF) in the Marmara region is composed of three par...
High-resolution 3-D seismic data acquired in the Sea of Marmara on the Western High, along the north...
[1] High-resolution 3-D seismic data acquired in the Sea of Marmara on the Western High, along the n...
The distribution of plate motion between multiple fault strands and how this distribution may evolve...
The Aegean region is one of the most rapidly deforming continental areas in the world. In the Sea of...
International audienceThe North Anatolian Fault experienced large earthquakes with 250-400 years rec...
The submerged portions of the North-Anatolian Fault (NAF) in the Sea of Marmara and the NE-Aegean Se...
International audienceAbstract A new analysis of high-resolution multibeam and seismic reflection da...
International audienceThe distribution of plate motion between multiple fault strands and how this d...
International audienceThe Sea of Marmara (SoM) is affected by large earthquakes occurring on the Nor...
Geodetic monitoring and patterns of seismicity indicate that the Northern Branch of the North Anatol...
Since the 1999 Izmit-Kocaeli earthquake, the Main Marmara Fault (MMF) of the North Anatolian Fault s...
The North Anatolian Fault (NAF) zone is 1500 km long, extending almost up to the Greek mainland in t...
International audienceThe North Anatolian Fault (NAF) in the Marmara region is composed of three par...
High-resolution 3-D seismic data acquired in the Sea of Marmara on the Western High, along the north...
[1] High-resolution 3-D seismic data acquired in the Sea of Marmara on the Western High, along the n...
The distribution of plate motion between multiple fault strands and how this distribution may evolve...
The Aegean region is one of the most rapidly deforming continental areas in the world. In the Sea of...
International audienceThe North Anatolian Fault experienced large earthquakes with 250-400 years rec...
The submerged portions of the North-Anatolian Fault (NAF) in the Sea of Marmara and the NE-Aegean Se...
International audienceAbstract A new analysis of high-resolution multibeam and seismic reflection da...
International audienceThe distribution of plate motion between multiple fault strands and how this d...
International audienceThe Sea of Marmara (SoM) is affected by large earthquakes occurring on the Nor...
Geodetic monitoring and patterns of seismicity indicate that the Northern Branch of the North Anatol...
Since the 1999 Izmit-Kocaeli earthquake, the Main Marmara Fault (MMF) of the North Anatolian Fault s...
The North Anatolian Fault (NAF) zone is 1500 km long, extending almost up to the Greek mainland in t...
International audienceThe North Anatolian Fault (NAF) in the Marmara region is composed of three par...