A5011716765- Marine and environmental studies
- earthquake and tectonic studies
- Maritime and Coastal Archaeology
- Hydrocarbon exploration and reservoir analysis
- Hydraulic Fracturing and Reservoir Analysis
- Geology and Paleoclimatology Research
- Seismic Imaging and Inversion Techniques
- Metallurgy and Cultural Artifacts
- Geochemistry and Geologic Mapping
- Drilling and Well Engineering
- Geological and Geochemical Analysis
- Geological formations and processes
- Seismology and Earthquake Studies
- Seismic Waves and Analysis
- Cultural and Sociopolitical Studies
- Pleistocene-Era Hominins and Archaeology
- Earthquake Detection and Analysis
- Energy and Environment Impacts
- Advanced X-ray and CT Imaging
- Fish Biology and Ecology Studies
- Historical Turkish Studies
- Geological Studies and Exploration
- High-pressure geophysics and materials
- Spectroscopy and Chemometric Analyses
- Geophysics and Gravity Measurements
Istanbul Technical University
2000-2022
Sivas State Hospital
1999
Antalya IVF
1999
Teknoloji Arastirma ve Gelistirme Endustriyel Urunler Bilisim Teknolojileri San Tic
1999
The Tekirdağ depression within the Marmara Sea in Mediterranean region is an active, rhomb‐shaped strike‐slip basin along North Anatolian fault with a floor at water depth of −1150 m. New multichannel seismic reflection data and on‐land geological studies indicate that forming releasing bend filled syntransform sediments Pliocene‐Quaternary age. bounded on one side by other subparallel normal fault, which forms steep submarine slope. In cross section strongly asymmetric thickness strata...
Research Article| May 01, 2012 Evidence for widespread creep on the flanks of Sea Marmara transform basin from marine geophysical data D.J. Shillington; Shillington * 1Lamont-Doherty Earth Observatory Columbia University, Palisades, New York 10964, USA *E-mail: djs@ldeo.columbia.edu. Search other works by this author on: GSW Google Scholar L. Seeber; Seeber C.C. Sorlien; Sorlien 2Earth Institute, University California, Santa Barbara, California 93106, M.S. Steckler; Steckler H. Kurt; Kurt...
The distribution of plate motion between multiple fault strands and how this may evolve remain poorly understood, despite the key implications for seismic hazards. North Anatolian Fault in northwest Turkey is a prime example multistranded continental transform. Here we present first constraints on late Quaternary slip rates its northern branch across Cinarcik Basin eastern Marmara Sea. We use both deep penetration high‐resolution multichannel reflection data with stratigraphic age model to...
The disastrous 1999 earthquakes in Turkey have spurred the international community to study geometry and behavior of North Anatolian Fault (NAF) beneath Marmara Sea. While area is considered mature for a large earthquake, detailed fault below Sea uncertain, this prevents realistic assessment seismic hazards highly‐populated region close Istanbul. Two geological/geophysical surveys were recently conducted Sea: first November 2000 with R/V Odin Finder , second June 2001 CNR‐Urania . Both...
Lake Sapanca is located in the Eastern Marmara region of Turkiye and formed as a tectonic lake by right-lateral strike slip North Anatolian Fault (NAF). Located 33 m above sea level, this has length 16 km east-west direction 5 north-south direction. The area which on Izmit-Sapanca Corridor, bordered segments northern branch NAF, between Samanlı Mountains to south Kocaeli Peneplain north. Multibeam bathymetry high-resolution seismic data were acquired part TUBITAK project (Project...
The gulf of Izmit is located at the eastern Marmara Sea and has an east-west elongated rectangular shape with about 60 km length in direction 2-10 width north-south (Figure 1). comprised three basins, from west to east, western (Darica), central (Karamursel), (Izmit) basins. basin connected other basins by two shallow sills north Hersek peninsula Golcuk 55 38 m water depths, respectively. centrally Karamursel constitutes deepest part Gulf a maximum depth 205 m.
Amplitude Versus Angle (AVA) modeling has been performed to find out effects of porosity and fluid type three different reservoir rock types. We used two layer earth models with shale/limestone, shale/sandstone shale/shaly sandstone horizontal interfaces. Our upper consists nonpermeable shale unit lower permeable rocks percentage porosities. Each interface is modeled assumption porosities 10%, 20% 30%. Reservoir are assumed gas, oil brine saturated. AVA gathers were created by using the...