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Assessment of earthquake hazard in Turkey and neighboring
Seismic hazard assessment Turkey earthquake UN/IDNDR Aegean sea North-Anatolian Fault
2015/9/30
The aim of this study is to conduct a probabilistic seismic hazard analysis for Turkey and neighboring regions, using the most recently developed attenuation relationships. The seismicity database is ...
Source parameters of the Izmit-Bolu 1999 (Turkey) earthquake sequences from teleseismic data
source inversion complex earthquake North Anatolian Fault
2015/9/28
Body waveform modelling and far-field displacement spectral analyses were used to study the source parameters of five of the largest earthquakes of the (Izmit-Bolu) Turkey 1999 sequence. The derived s...
Numerical 2D modeling of site responsein Dinar Graben, Southwest Turkey,and comparison with observations
2D modeling basin edge effect Dinar site response
2015/9/10
The October 1, 1995 Dinar earthquake (ML=5.9) caused extensive damage within a limited area in Dinar town located
in southwestern Turkey. Graben structure of the damaged area suggests the basin edge ...
Local earthquake tomography of the Erzincan Basin and the surrounding area in Turkey
local earthquake tomography Erzincan Basin 3D velocity structure
2015/9/2
In this study, selected travel time data from the aftershock series of the Erzincan earthquake (March, 1992, Ms=6.8) were inverted simultaneously for both hypocenter locations and 3D Vp and Vs structu...
A ground radiometric study of uranium,thorium and potassium in Isparta,Turkey
ground radiometric uranium thorium potassium Isparta Turkey
2015/8/28
The radioelement concentrations of uranium (238U), thorium (232Th) and potassium (40K), as their radionuclides eU, eTh and K, of Cünür Hill in the city of Isparta (Turkey) and its surroundings were me...
Paleoseismic record obtained by coring a sag-pond along the North Anatolian Fault (Turkey)
Paleoseismology seismites sedimentary cores North Anatolian Fault
2015/8/26
Shallow lakes along minor structural bends or discontinuities of strike-slip faults are not usually paleoseismological target sites. In the present study, we show that a 2-m-deep, 700-m-long lake that...
Submarine Paleoseismology Along Populated Transform Boundaries: The Enriquillo-Plantain-Garden Fault, Canal du Sud, Haiti, and the North Anatolian Fault, Marmara Sea, Turkey
Populated Transform Boundaries Submarine Paleoseismology
2015/7/17
Continental transform boundaries cross heavily populated regions and are associated with destructive earthquakes worldwide. The devastating 1999 Turkey earthquakes and the offshore 2010 Haiti earthqua...
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...
The October 20, 2006 Manyas (ML=5.2) and October 24, 2006 Gemlik (ML=5.2) earthquakes in the Marmara region (NW Turkey): ground motion characteristics
Earthquake GPS Historical seismology Ionosphere Irpinia
2015/8/18
In this study, we analyze the ground motion characteristics of October 20, 2006 Manyas (ML=5.2) and October 24, 2006 Gemlik (ML=5.2) earthquakes. Both earthquakes occurred on the southern branch of th...
Evidence for Damaging Historical Earthquakes at Priene, Western Turkey
Earthquakes Western Turkey Priene
2009/7/8
The ancient cilty of Priene was one of the earliest Ionian settlements within the western part of the Büyük Menderes valley (the ancient Maeander River) and was first founded about 8 km in the east of...
Geochronology and Geochemistry of Basaltic Rocks in The Karasu Graben Around Kırıkhan (Hatay), S. Turkey
Continental Rift Zone Geochemistry Geochronology Basaltic Rocks
2009/7/8
The study area, which is located in the middle sector of the Amanos mountains, covers the north of Kırıkhan (Hatay) in southern Turkey. Tectonostratigraphic rock units from Paleozoic to Ceno...
The June 6, 2000, Orta (Çankırı, Turkey) Earthquake: Sourced from a New Antithetic Sinistral Strike-slip Structure of the North Anatolian Fault System, the Dodurga Fault Zone
North Anatolian Fault System Antithetic Fault Sinistral Strike-slip Fault Orta Earthquake
2009/7/8
The İsmetpaşa-Kargı section of the North Anatolian Fault System (NAFS) consists of six subfault zones, namely the Eskipazar, the Ulusu, the Tosya, the Çerkeş-Kurşunlu, ...
Earthquake Faulting at Ancient Cnidus, SW Turkey
Cnidus archaeoseismology faulting surface rupture earthquake
2009/7/8
The ruins of Cnidus, an important ancient city in southwestern Asia Minor, lie directly on an earthquake fault - the Cnidus Fault. Offset and deformed archaeological remains along the trace of the fau...
Extensional Neotectonic Regime through the NE Edge of the Outer Isparta Angle, SW Turkey: New Field and Seismic Data
Akş ehir-Afyon Graben Isparta Angle extensional neotectonic regime Sultandağ ı and Ç ay (Afyon) earthquakes
2009/7/8
The Akşehir-Afyon Graben (AAG) is a 4-20-km-wide, 130-km-long NW-trending depression that separates central Anatolia in the NE and the Isparta Angle (IA) in the SW. Its southwestern margin-boundi...
Water-Level Changes in Shallow Wells Before and After the 1999 İzmit and Düzce Earthquakes and Comparison with Long-Term Water-Level Observations (1999–2004), NW Turkey
ground-water well-level changes earthquake forecast continental deformation North Anatolian Fault Zone Thrace-Eskiş ehir Fault Zone 1999 İ zmit-Düzce earthquakes
2009/7/7
It is well known that earthquakes cause hydrological changes, such as drying or flooding of water wells, fluctuations in ground-water levels in wells, changes in water quality, and formation of new sp...