A5045088311- Geological Formations and Processes Exploration
- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Geology and Environmental Impact Studies
- Hydrocarbon exploration and reservoir analysis
- Rock Mechanics and Modeling
- Ancient and Medieval Archaeology Studies
- Geotechnical and Mining Engineering
- Historical and Archaeological Studies
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Geotechnical and Geomechanical Engineering
- Seismic Imaging and Inversion Techniques
- Geological Studies and Exploration
- Drilling and Well Engineering
- Geology and Paleoclimatology Research
University of Warsaw
2016-2024
Tectonic inversion and erosion conceal basin geological history. As simple stratigraphic reconstructions can be inaccurate, thermal modelling techniques are often applied. In this paper, we show the advantages of a multi-proxy approach for exhumation studies, which explores full range all possible solutions. The part Mesozoic Central European Basin that was inverted into Mid-Polish Anticlinorium in Late Cretaceous is chosen as case study. analysis consists three steps: First, wide scenarios...
Research Article| November 01, 2016 Formation of intracontinental basins in the opposite corners Tabas block as coeval structures controlled by transpressional faulting, Iran Andrzej Konon; Konon † 1Faculty Geology, University Warsaw, Żwirki i Wigury 93, PL-02-089 Poland †andrzej.konon@uw.edu.pl Search for other works this author on: GSW Google Scholar Alireza Nadimi; Nadimi 2Department Faculty Science, Isfahan, P.O. Box 81746-73441, Marek Koprianiuk; Koprianiuk 3Polish Oil and Gas Company...
Abstract A newly recognized Mnin restraining stepover is identified in the Permo-Mesozoic cover of western part Late Palaeozoic Holy Cross Mountains Fold Belt (Poland), within a fault pattern consisting dextral strike-slip faults. The formation large contractional structure at Cretaceous – Cenozoic transition displays significant role faulting along border Teisseyre-Tornquist Zone, foreland Polish Carpathian Orogen. Theoretical relationships between maximum offsets/ mean step length, as well...
Bed-parallel veins that originated in organic-rich laminated rocks are considered to be related organic matter (OM) content. The presence of OM and lamination affects the properties host increases bulk rock anisotropy. occurring lower Palaeozoic mudstone formations northern part Polish Caledonian Foredeep Basin were previously interpreted as having been formed a result horizontal shortening. present work extends study area c. 65 km south previous investigations identify factors influenced...
Recognition of fractures and faults related to different types folding is important for understanding how fluids flow in folds or which parts represent a better productive sector reservoirs due to, example, changes the intensity distribution fractures. In this paper, we suggest that seismic data alone may be insufficient determine style buckle folding. The differences mechanical properties rock masses favour development two main internal deformation within folds, originated as result...
Abstract In a recently published report focused on the role of swelling Triassic clays as dominant process that led to local steepening competent Jurassic strata, its authors presented an opinion lack evidence for existence Gnieździska–Brzeziny strike‐slip fault along contact between and rocks. This discussion presents structural, geophysical, cartographic geomechanical data indicating rocks is defined by vertical dextral fault, which was formed after tilting beds in Late Cretaceous. The...
The damage zones of exhumed strike-slip faults dissecting Jurassic carbonates in the south-western part Late Palaeozoic Holy Cross Mountains Fold Belt reveal second-order and fractures infilled with syntectonic calcite. subsequent development a structural pattern microscopic fault-related structures calcite infillings reflects activity that began Cretaceous (Late Maastrichtian) lasted until early Miocene (Langhian). fabric veins provides insights into evolution permeable were main pathways...
Summary The study focuses on an integrated analysis of stress directions and magnitudes for a deep borehole (D-1) located in the active orogen. integration available geophysical data allowed as to distinguish three structural units penetrated by investigated borehole, which were taken into account geomechanical modelling. developed SigmaG software us determine (1D Mechanical Earth Model) within D-1 assuming linearly variable strain values recognized tectonic units. additionally checked...