indicating a
transtenstional geotectonic regime (Pavlides & Caputo,
1994). NAT consists of two large, roughly parallel and
opposite fault zones that cross and affect the sea-floor of
the eastern part of the North Aegean Sea (Caputo et al.,
2013), while NAB is directly connected with the NAT,
although there is a slight geometric, behavioural and
morphological change that can be observed N-NNW
from Lemnos Island. The main active tectonic structures
in the study area are described by Chatzipetros et al.
(2013) and can be found in the Greek Database of
Seismogenic Sources (GreDaSS; Figure 1; Caputo et al.,
2013). The main types of seismogenic sources included
in GreDaSS are (according to Basili et al. 2008, and
Sboras 2012):
indicating a
transtenstional geotectonic regime (Pavlides & Caputo,
1994). NAT consists of two large, roughly parallel and
opposite fault zones that cross and affect the sea-floor of
the eastern part of the North Aegean Sea (Caputo et al.,
2013), while NAB is directly connected with the NAT,
although there is a slight geometric, behavioural and
morphological change that can be observed N-NNW
from Lemnos Island. The main active tectonic structures
in the study area are described by Chatzipetros et al.
(2013) and can be found in the Greek Database of
Seismogenic Sources (GreDaSS; Figure 1; Caputo et al.,
2013). The main types of seismogenic sources included
in GreDaSS are (according to Basili et al. 2008, and
Sboras 2012):
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