A5016265254- Geological Formations and Processes Exploration
- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Marine and environmental studies
- earthquake and tectonic studies
- Mineralogy and Gemology Studies
- Radioactive element chemistry and processing
- Geological Studies and Exploration
- Soil and Environmental Studies
- Nuclear Physics and Applications
- Remote Sensing and Land Use
- Advanced X-ray and CT Imaging
- Nuclear reactor physics and engineering
- Regional Development and Management Studies
- Landslides and related hazards
- Soil erosion and sediment transport
- Community Development and Social Impact
- Analytical chemistry methods development
- Mass Spectrometry Techniques and Applications
- Paleontology and Stratigraphy of Fossils
- Geotechnical and Geomechanical Engineering
- Methane Hydrates and Related Phenomena
- Remote-Sensing Image Classification
- Nuclear Materials and Properties
University of Belgrade
2004-2024
University of Belgrade - Faculty of Mining and Geology
2024
Quantitative techniques for spatial prediction and classification in geological survey are developing rapidly. The recent applications of machine learning confirm possibilities their application this field research. paper introduces Support Vector Machines, a method derived from achievements the statistical theory, units based on source Landsat multispectral images. initial experiments suggest usefulness proposed approach.
In the tectonic setting of Dinaric-Hellenic belt, Vardar Zone is represented by a NW-SE to N-S striking assemblage oceanic and continental units, each showing different metamorphic grade deformation features. this paper, detailed description stratigraphic structural features units cropping out in Kopaonik area, belonging Serbia, presented. addition, 1:50.000 scale geological map studied area also provided. present stack originated during Alpine phases referred both External Central Zones...
Abstract The easternmost zone of the Dinaric‐Hellenic belt is represented by Vardar Zone, in which Kopaonik Metamorphic Complex (KMC) regarded as lowermost unit. This complex topped unmetamorphosed Brzece unit and intruded Oligocene Intrusive complex. KMC characterized a stratigraphy that includes metapelites meta‐carbonates Late Triassic age, associated with metabasites. It deformation history comprises four phases: D1 to D4. phase structures occur only relict structures, whereas D2 are...
This study presents and discusses new data about the lithology deformation style of Bukulja-Lazarevac Palaeozoic Unit (BLPz) compares its characteristics to those exhibited by adjacent units complex suture central Balkan Peninsula, namely: Drina-Ivanjica (DIU), Jadar Block (JBU) Diaina (DPz) Units. The BLPz consists four metasedimentary metaigneous formations metamorphosed under greenschist facies conditions. Only rare rocks show evidences an earlier metamorphism amphibolites is...
Abstract In this study we performed a calculation of the tectonic stress tensor based on fault slip data and all available focal mechanisms in order to determine principal axes recent regime westernmost unit Getic nappe system (Gornjak-Ravanica Zone, Eastern Serbia). The is combined dataset involving paleostress analyses, inversion remote sensing. results show dominant strike-slip kinematics with maximal compression axis oriented NNE-SSW. This compatible northward motion counterclockwise...
Volcano-sedimentary basins located in the orogenic hinterland area overlying subducted slabs are observed worldwide to be driven by switching tectonic regimes induced changing mechanics of slab. Despite many qualitative studies, quantitative link between slab?s and basins? evolution is less understood. Among examples worldwide, Timok Magmatic Complex (TMC) Serbia represents an optimal natural laboratory due complex setting during various stages Middle Jurassic-Paleogene subduction system....
Among the many examples observed worldwide, Timok Magmatic Complex (TMC) basin of Serbian Carpathians represents an excellent area for a process-oriented study on interplay between tectonics, sedimentation, and magmatism in continental back-arc basins above evolving subducted slabs. The TMC is segment larger Late Cretaceous Apuseni-Banat-Timok-Srednogorie (ABTS) magmatic belt, formed response to subduction Mesozoic Neotethys oceanic lithosphere beneath Carpatho-Balkanides south-eastern...
Abstract Ensuring the quality protection of geospatial elements entails environmental control, a task unattainable without precise measurement results. This article aims to conduct spatio-temporal analysis soil degradation and vegetation status within influence zone Kolubara Mining Basin in Serbia. Remote sensing is employed assess vulnerability erosion using potential method. A geographic information system environment utilized generate an map, illustrating erosive processes across...
The Serbo-Macedonian Massif (SMM) represents a composite crystalline terrane situated between the two diverging branches of the Eastern Mediterranean Alpine orogenic system, northeast-vergent Carpatho- Balkanides and southwest-vergent Dinarides Hellenides. It is outcropping from Pannonian basin in north, to the Aegean Sea south, along central and southeastern Serbia, southwestern Bulgaria, eastern Macedonia Greece. Its affiliation European and/or African plate basement still...