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dc.contributor.authorOnal, K. Mert
dc.contributor.authorBuyuksarac, Aydin
dc.contributor.authorAydemir, Attila
dc.contributor.authorAtes, Abdullah
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T10:14:53Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T10:14:53Z
dc.date.issued2008
dc.identifier.issn0040-1951
dc.identifier.issn1879-3266
dc.identifier.urihttps://dx.doi.org/10.1016/j.tecto.2008.08.006
dc.identifier.urihttps://hdl.handle.net/20.500.12418/10288
dc.descriptionWOS: 000261283100015en_US
dc.description.abstractSivas Basin is the easternmost and third largest basin of the Central Anatolian Basins. In this study, gravity, aeromagnetic and seismic data are used to investigate the deep structure of the Sivas Basin, together with the well seismic velocity data, geological observations from the surface and the borehole data of the Celalli-1 well. Basement depth is modeled three-dimensionally (3D) using the gravity anomalies, and 2D gravity and magnetic models were constructed along with a N-S trending profile. Densities of the rock samples were obtained from the distinct parts of the basin surface and in-situ susceptibilities were also measured and evaluated in comparison with the other geophysical and geological data. Additionally, seismic sections, in spite of their low resolution, were used to define the velocity variation in the basin in order to compare depth values and geological cross-section obtained from the modeling studies. Deepest parts of the basin (12-13 km), determined from the 3D model, are located below the settlement of Hafik and to the south of Zara towns. Geometry, extension and wideness of the basin, together with the thickness and lithologies of the sedimentary units are reasonably appropriate for further hydrocarbon exploration in the Sivas Basin that is still an unexplored area with the limited number of seismic lines and only one borehole. (c) 2008 Elsevier B.V. All rights reserved.en_US
dc.description.sponsorshipTUBITAK [106Y301]en_US
dc.description.sponsorshipAuthors would like to thank the General Directorate of Mineral Research and Exploration (MTA) of Turkey for providing borehole, aeromagnetic and gravity data. Seismic sections were provided by the General Directory of Petroleum Affairs (GDPA). This research was financially supported by TUBITAK (Project Code: 106Y301). Authors would like to thank Mr. Serdar Demiralin for reading and critiquing the manuscript before submission. Authors extend their thanks to the editor jean-Pier Burg and an anonymous reviewer for their constructive critiques. Thanks are also for the journal Manager Andres Villavicencio for his friendly efforts.en_US
dc.language.isoengen_US
dc.publisherELSEVIER SCIENCE BVen_US
dc.relation.isversionof10.1016/j.tecto.2008.08.006en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectSivas Basinen_US
dc.subjectKangal Basinen_US
dc.subjectGravity anomalyen_US
dc.subjectAeromagnetic anomalyen_US
dc.subject2D and 3D modelingen_US
dc.subjectCelalli-1 wellen_US
dc.titleInvestigation of the deep structure of the Sivas Basin (innereast Anatolia, Turkey) with geophysical methodsen_US
dc.typearticleen_US
dc.relation.journalTECTONOPHYSICSen_US
dc.contributor.department[Aydemir, Attila] Turkiye Petrolleri AO, TR-06100 Ankara, Turkey -- [Onal, K. Mert] ITU Fac Mines, Dept Geophys Engn, TR-34469 Istanbul, Turkey -- [Buyuksarac, Aydin] Cumhuriyet Univ, Dept Geophys Engn, TR-58140 Sivas, Turkey -- [Ates, Abdullah] Ankara Univ, Dept Geophys Engn, TR-06100 Ankara, Turkeyen_US
dc.contributor.authorIDOnal, Kemal Mert -- 0000-0002-9046-1227en_US
dc.identifier.volume460en_US
dc.identifier.issue01.Apren_US
dc.identifier.endpage197en_US
dc.identifier.startpage186en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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