Geophysical model of the Tertiary basin between Čačak and Kraljevo [Serbia] | Геофизички модел геолошке грађе чачанско-краљевачког терцијарног басена [Србија]
2010
Младеновић, А., Рударско-геолошки факултет, Београд (Serbia)
Research was done with the task of determining geophysical and tectonic characteristics of the Tertiary basin between Čačak and Kraljevo, in order to develop subsurface model of this basin. In respect to defined tasks, analysis of gravity and geomagnetic maps and Landsat 7 satellite image, were done. It was determined that the basin was made of Tertiary and Quaternary sediments, which are 800-1200 meters thick. Basis of these sediments is made of serpentinite and serpentinized peridotite. Also, an origin of positive Bouguer anomaly, which is situated in western part of investigated area, was proposed. Two families of ruptures are dominating on the investigated area. First family, of the northwest-southeast stretch is one by which basin has been formed. The second family, of the southwest-northeast stretch, is one by which eruption of andesite has been done.
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