Metallogeny of the simav graben (Inner-Western Anatolia, Turkey)

Download
068306.pdf
1997
Oygür, Vedat
Show full item record
237
views
0
downloads
Grabens(Geology), Geology, Structural, Metallogeny.
https://hdl.handle.net/11511/1088
Graduate School of Natural and Applied Sciences, Thesis

Suggestions

Neotectonics and evolution of the Eskipazar Basin, Karabük ا Turkey
Biryol, C. Berk; Koçyiğit, Ali; Department of Geological Engineering (2004)
Study area, the Eskipazar Basin, is located in the western part of the North Anatolian Fault System. It is a 3-5 km wide, 10 km long and NWSE trending depression, bounded by a complex array of oblique-slip normal faults and strike-slip faults. The Eskipazar Basin is interpreted to be a superimposed basin. The basin fill is composed of two different units deposited under the control of different tectonic regimes, namely the paleotectonic and the neotectonic regimes. The latest paleotectonic fill of the basin...
Post miocene deformation of the area between Alibey (Kızılcahamam) and Karalar (Kazan) villages, nw Ankara (Turkey)
Karaca, Aykut; Rojay, Fuat Bora; Department of Geological Engineering (2004)
The study area is located within the Neogene-Quaternary sequences on top of the Mesozoic accreted mass at the northwest of Kazan (40 km NW of Ankara) between Karalar and Alibey villages. The research deals with the post-Miocene deformational history of an area situated at the southern edge of Galatian Volcanic Province. Two main Neogene rock sequences are cropped out; 1) Late Miocene Pazar Formation, 2) Plio-Quaternary Sinap Formation. The Pazar Formation has a succession composed mainly of clastics at the ...
Neotectonics and evolution of the yeniçağ basın, Bolu-Turkey
Arca, M Serkan; Koçyiğit, Ali; Department of Geological Engineering (2004)
Study area, the Yeniçaga Basin, is located in the western part of the North Anatolian Fault System. It is a 1-5-km-wide and 14-km-long WSWENE- trending depression bounded by a complex array of strike-slip faults. The Yeniçaga Basin is interpreted to be a fault ا wedge basin with the North Anatolian Fault̕s System Master Strand, namely the Gerede Fault, cutting across the basin itself. The basin and its surroundings contain mainly two groups of rock units namely the paleotectonic units and the neotectonic un...
Neotectonics and seismicity of the Ankara region : a case study in the Uruş area
Kaplan, Tülin; Koçyiğit, Ali; Department of Geological Engineering (2004)
Study area, the Urus province, is located 70 km WNW of city of Ankara. Major settlements in the study area are two counties, Urus and Güdül; and there are a number of villages, such as, from W to E, Macun, Yogunpelit, Kabaca, Üregil, Özköy, Tahtaciörencik, Kirkkavak, Kavaközü, Kayi and Karacaören. The study area is 189 km2 in size and included in 1/25000-scaled topographic quadrangles of H28a3, a4, d1 and d2. The Güdül- Urus section of the Çeltikçi morphotectonic depression (Çeltikçi Basin) drained by the A...
Remote sensing study of sürgü fault zone(Malatya, Turkey)
Koç, Ayten; Kaymakcı, Nuretdin; Department of Geodetic and Geographical Information Technologies (2005)
The geometry, deformation mechanism and kinematics of the Sürgü Fault Zone is investigated by using remotely sensed data including Landsat TM and ASTER imagery combined with SRTM, and stereo-aerial photographs. They are used to extract information related to regional lineaments and tectono-morphological characteristics of the SFZ. Various image processing and enhancement techniques including contrast enhancement, PCA, DS and color composites are applied on the imagery and three different approaches includin...
Citation Formats
V. Oygür, “Metallogeny of the simav graben (Inner-Western Anatolia, Turkey),” Ph.D. - Doctoral Program, Middle East Technical University, 1997.
METU IIS - Integrated Information Service open@metu.edu.tr