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Paleoseismological investigations on a slow-moving active fault in central Anatolia, Tecer Fault, Sivas
paleoseismology earthquake slow-moving fault central Anatolia
2015/8/26
Tecer Fault is a N60˚-70˚E-trending, left-lateral, strike-slip fault to the south of the town of Sivas, Turkey. This fault is considered as the eastward continuation of Deliler Fault, which ...
Jurassic–Paleogene intraoceanic magmatic evolution of the Ankara Mélange, north-central Anatolia, Turkey
Jurassic–Paleogene interoceanic magmatic evolution the Ankara Melange north-central Anatolia Turkey
2015/1/6
Oceanic rocks in the Ankara Mélange along the Izmir–Ankara–Erzincan suture zone (IAESZ) in north-central Anatolia include locally coherent ophiolite complexes (~ 179 Ma and ~ 80̷...
Monitoring the Kinematics of Anatolia Using Permanent GPS Network Stations
permanent GPS networks Anatolia coseismic deformation postseismic deformation
2009/7/8
The establishment and promotion of three-dimensional geodetic networks supported by continuous Global Positioning System (GPS) data are capable of yielding valuable data in order to enable regional r...
Crustal Structure of the Eastern Part of Central Anatolia (Turkey)
crustal structure magnetotelluric sutures Central Anatolia Turkey
2009/7/7
This study aims to examine crustal structure in the eastern part of central Anatolia using the magnetotelluric (MT) method. MT data have been collected from 37 stations along a north-south 220 km prof...
Isostatic Compensation in Western Anatolia with Estimate of the Effective Elastic Thickness
effective elastic thickness isostatic response functions gravity Western Anatolia admittance analysis
2009/7/7
Isostasy is concerned with how the crust and mantle adjusts to shifting loads of limited spatial and temporal dimensions. By analysing the frequency content of gravity and topography data, it has been...
Statistical Earthquake Frequency Analysis for Western Anatolia
extreme value distribution Western Anatolia zonation seismic assessment earthquake
2009/7/7
In order to apply a statistical earthquake frequency analysis to western Anatolia, the area has been restricted within coordinates 36.50º-40º North and 26.00º-30.00º East. Data use...