A5050518428- Geological Formations and Processes Exploration
- Geological formations and processes
- Geology and Paleoclimatology Research
- Hydrocarbon exploration and reservoir analysis
- Geological Studies and Exploration
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Pleistocene-Era Hominins and Archaeology
- Paleontology and Stratigraphy of Fossils
Czech Geological Survey
2009-2012
Czech Academy of Sciences, Institute of Geology
2008-2012
Charles University
2005-2012
ABSTRACT The Oligo‐Miocene Most Basin is the largest preserved sedimentary basin within Eger Graben, easternmost part of European Cenozoic Rift System (ECRIS). interpreted as a an incipient rift system that underwent two distinct phases extension. first phase, characterised by NNE–SSW‐ to N–S‐oriented horizontal extension between end Eocene and early Miocene, was oblique axis caused evolution fault en‐échelon‐arranged E–W (ENE–WSW) faults. These faults defined number small, shallow initial...
Abstract The Early Miocene Bílina Palaeodelta consists of fluvio‐deltaic and lacustrine clastics deposited along the south‐eastern margin extensional Most Basin, part Eger Graben in north Bohemia (Czech Republic). succession shows evidence repeated advances an axial deltaic system across a thick accumulation organic material clay hangingwall active fault. Exposures up to ca 4·5 km long open‐cast mine help bridge gap between seismic scale typical outcrop observation thus allow relationships...
Abstract This paper illustrates the response of a fluvial depositional system to interplay between peat compaction and clastic sediment supply, at range spatial temporal scales, as documented by extensive exposures in an open‐cast mine Most Basin, part Oligo‐Miocene Ohře Rift (Eger Graben) basin Czech Republic. The Basin is characterized occurrence number phenomena resulting from syn‐ post‐depositional interactions sedimentary systems underlying accumulation organic material that was...
The basal Ordovician Třenice Formation represents an initial unit of the preserved infill Prague Basin.Volcanic admixture in sediments south-western part basin suggests subaerial volcanic activity during deposition Formation.Three principal lithofacies associations were defined within sedimentary record based on petrography and observed structures: i) graded conglomerates, ii) lithic sandstones iii) volcanigenic deposits.The studied mostly deposited as subtidal sand dunes, locally...
The present-day geological and morphological expression of the Cenozoic Eger Rift in central Europe is dominated by faulted edge Krušné Hory (Erzgebirge) Mts., a plateau uplifted to c. 1 km above sea level following mid-Miocene, resulting partial deformation erosion parts sedimentary volcanic infill. main phase uplift considered have occurred Plio-Quaternary times, but details this process its relation itself remain unclear. Oligo – Miocene Most Basin most...