dc.contributor.author | Rozimant, Kamil | |
dc.contributor.author | Buyuksarac, Aydin | |
dc.contributor.author | Bektas, Oezcan | |
dc.date.accessioned | 2019-07-27T12:10:23Z | |
dc.date.accessioned | 2019-07-28T10:14:29Z | |
dc.date.available | 2019-07-27T12:10:23Z | |
dc.date.available | 2019-07-28T10:14:29Z | |
dc.date.issued | 2009 | |
dc.identifier.issn | 0033-4553 | |
dc.identifier.issn | 1420-9136 | |
dc.identifier.uri | https://dx.doi.org/10.1007/s00024-009-0447-8 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12418/10188 | |
dc.description | WOS: 000264884700008 | en_US |
dc.description.abstract | The magnetic map of Slovakia used in the paper was compiled as part of a project titled Atlas of Geophysical maps and profiles in 2001. The residual magnetic data were analyzed to produce Curie point estimates. To remove distortion of magnetic anomalies caused by the Earth's magnetic field, reduction to pole transformation was applied to the magnetic anomalies using the magnetization angle of the induced magnetization. Anomalies reduced to the pole tend to be better correlated with tectonic structures. We applied a 3-km upward continuation to the residually compiled magnetic anomalies in order to remove effects of topography. The depth of magnetic dipoles was calculated by an azimuthally averaged power spectrum method for the entire area. Such estimates can be indicative of temperatures in the crust, since magnetic minerals lose their spontaneous magnetization according to Curie temperature of the dominant magnetic minerals in the rocks. The computed Curie point depths in the Slovakia region vary between 15.2 km and 20.9 km. Heat flow higher than 100 mWm(-2) occurs at the central volcanics and eastern part of Slovakia, where the Curie point depths values are shallow. The correlation between Curie point depths, heat flow and crust depth was investigated for two E-W cross sections. Heat flow and Curie point depth values are correlated with each other however, these values could not be correlated with crust depth. The Curie point isotherm, which separates magnetic and non-magnetic parts of the crust, is represented in two cross sections. | en_US |
dc.description.sponsorship | Slovak Academic Information Agency (SAIA) | en_US |
dc.description.sponsorship | The authors thank the anonymous referee for her/his suggestions and corrections on the manuscript. We thank the State Geological Institute of Dionyz Stur for providing aeromagnetic data. Dr. Aydin Buyuksarac extends gratitude to the Slovak Academic Information Agency (SAIA) for Grant and Comenius University in Bratislava, Department of Engineering and Environmental Geophysics for their hospitality. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | SPRINGER BASEL AG | en_US |
dc.relation.isversionof | 10.1007/s00024-009-0447-8 | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject | Magnetic anomalies | en_US |
dc.subject | neogene volcanics | en_US |
dc.subject | power spectrum | en_US |
dc.subject | Curie point depth | en_US |
dc.subject | Magnetized crust | en_US |
dc.title | Interpretation of Magnetic Anomalies and Estimation of Depth of Magnetic Crust in Slovakia | en_US |
dc.type | article | en_US |
dc.relation.journal | PURE AND APPLIED GEOPHYSICS | en_US |
dc.contributor.department | [Rozimant, Kamil] Comenius Univ, Fac Nat Sci, Dept Appl & Environm Geophys, Bratislava, Slovakia -- [Buyuksarac, Aydin] Cumhuriyet Univ, Fac Engn, Dept Geophys Engn, TR-58140 Sivas, Turkey -- [Bektas, Oezcan] Ankara Univ, Dept Geophys Engn, TR-06100 Ankara, Turkey | en_US |
dc.contributor.authorID | Bektas, Ozcan -- 0000-0001-5232-4654 | en_US |
dc.identifier.volume | 166 | en_US |
dc.identifier.issue | 3 | en_US |
dc.identifier.endpage | 484 | en_US |
dc.identifier.startpage | 471 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |