Jozef Madzin

Jozef Madzin
Earth Science Institute of the Slovak Academy of Sciences · Department of Geomagnetism, Paleomagnetic Laboratory

PhD.

About

8
Publications
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50
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Additional affiliations
September 2010 - August 2014
Comenius University Bratislava
Position
  • PhD Student

Publications

Publications (8)
Article
Full-text available
Anisotropy of magnetic susceptibility and anisotropy of anhysteretic remanent magnetization were studied in the Oligocene turbidites of the weakly deformed Central Carpathian Paleogene Basin. In order to decide whether the magnetic fabric can be related to deposition from a paleoflow or to incipient weak tectonic deformation we compared magnetic...
Article
The thin skinned Hronic nappe system represents the structurally highest tectonic unit in the Late Cretaceous thrust-stack of the Central Western Carpathians. It mostly comprises a Permian volcano-sedimentary sequence and Triassic carbonate sediments which crop out in different parts of the Central Western Carpathians. We carried out a systematic p...
Article
Full-text available
The Pieniny Klippen Belt contains thickening and coarsening upwards synorogenic sedimentary successions witnessing the collision of the Oravic ribbon continent with the Central Carpathian orogenic wedge after the closure of the Vahic Ocean in the Late Cretaceous to Early Palaeogene. The sedimentary record of this event is represented by flysch/wild...
Article
This paper presents geochemical data on sedimentary rocks from the Upper Cretaceous to Lower Eocene formations of the Pieniny Klippen Belt (Western Carpathians, Slovakia). On the basis of geochemical analyses of 15 samples, the plate tectonic setting of sediment accumulation and paleodepositional environment were reconstructed, which may help to un...
Article
Full-text available
Biostratigraphic investigations of carbonate strata that sandwich volcanic rocks and studies of the volcanic rocks were made along five composite lithological sections across the Upper Jurassic-Lower Cretaceous carbonate rocks of autochthonous cover of the High-Tatric Unit in the Osobita peak area of the Western Tatra Mts. A carbonate microbreccia...
Article
Full-text available
An exceptional, briefly exposed section across the boundary between the Pieniny Klippen Belt (PKB) and the Central Carpathian Paleogene Basin (CCPB) in Eastern Slovakia showed that the contact is formed by a single, subvertical fault plane. Whereas the Oligocene CCPB deposits exhibit only weak deformation with S-verging fold-and-thrust structures,...
Article
Conference title - 9. Vyrocny predvianocny seminar Slovenskej geologickej spolocnosti--9th Annual seminar of the Slovak Geological Society, Copyright - GeoRef in Process, Copyright 2013, American Geosciences Institute. After editing and indexing, this record will be added to Georef., Language of summary - English, Pages - 497, ProQuest ID - 8853205...

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