Bartosz Kurjanski
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View article: The Paso Anomaly: shallow gas contained within Lower Pleistocene glaciogenic deposits in the Central North Sea
The Paso Anomaly: shallow gas contained within Lower Pleistocene glaciogenic deposits in the Central North Sea Open
The perception of shallow gas accumulations has changed from one of ‘drilling hazards’ to ‘potential resources’ over the last few years. The Paso Anomaly, identified on seismic at a depth of c . 550 m true vertical depth subsea (TVDss), is…
View article: The role of shallow banks and marine ice domes in marine‐based ice‐sheet deglaciation
The role of shallow banks and marine ice domes in marine‐based ice‐sheet deglaciation Open
Marine‐based ice sheets are susceptible to collapse and faster retreat than their land‐terminating counterparts. One of the key factors contributing to the relative stability of marine‐terminating ice sheets is the presence of shallow bath…
View article: Marine Geohazards and Geo-Engineering Constraints on the Glaciated European Margins
Marine Geohazards and Geo-Engineering Constraints on the Glaciated European Margins Open
The glaciated European continental margins (spanning 49-82°N and 16°W-36°E) are home to a thriving offshore energy sector and densely inhabited coastal areas. These regions face numerous marine geohazards and geo-engineering challenges due…
View article: Geomorphological Analysis of Cirques in the Western Islands of Greenland
Geomorphological Analysis of Cirques in the Western Islands of Greenland Open
This study employs Arctic DEM data and GIS tools, ACME 2.0 (Li et al., 2024), and GlaRe (Pellietero et al., 2016), to systematically investigate cirques in the western islands off central Greenland. The primary objective is to reconstruct …
View article: Dynamic changes in depositional patterns and glaciotectonic deformations revealed by high-resolution 3D seismic data in the Northern North Sea.
Dynamic changes in depositional patterns and glaciotectonic deformations revealed by high-resolution 3D seismic data in the Northern North Sea. Open
During the Last Glacial Maximum (LGM), the British-Irish ice sheet is known to have been coalescent with the Fennoscandian ice sheet. Some models indicate that this might have been rather short-lived, whereas other reconstructions indicate…
View article: Effect of bathymetric data resolution on the understanding of sediment mobility: implications for offshore infrastructure projects on deglaciated continental shelves
Effect of bathymetric data resolution on the understanding of sediment mobility: implications for offshore infrastructure projects on deglaciated continental shelves Open
Sediment mobility is one of the key issues considered  during the design and construction process off offshore infrastructure ( Wind farms, cables, pipelines etc.).  Early understanding of the seabed mobility can significantly af…
View article: Cool deltas: Sedimentological, geomorphological and geophysical characterization of ice‐contact deltas and implications for their reservoir properties (Salpausselkä, Finland)
Cool deltas: Sedimentological, geomorphological and geophysical characterization of ice‐contact deltas and implications for their reservoir properties (Salpausselkä, Finland) Open
Sediments deposited by glacial meltwaters (for example, ice‐contact delta deposits) form permeable packages in the subsurface that can act as reservoirs for both water and hydrocarbons. They are also an important source of aggregate for th…
View article: Ice-contact deltas investigation using ground penetrating radar (GPR), sedimentology, electrical resistivity tomography (ERT) and , Salpausselka I and II near Lahti, Finland
Ice-contact deltas investigation using ground penetrating radar (GPR), sedimentology, electrical resistivity tomography (ERT) and , Salpausselka I and II near Lahti, Finland Open
<p>In Finland, two large &#8220;moraine&#8221; ridges (Salpausselka I and Salpausselka II), extending to over 600 km in length, delineate two major stillstand/readvance positions of the Fennoscandian ice sheet during the last…
View article: Morphological evidence for marine ice stream shutdown, central Barents Sea
Morphological evidence for marine ice stream shutdown, central Barents Sea Open
Marine-based ice streams are responsible for a significant proportion of the ice mass loss from the present-day Greenland Ice Sheet, East Antarctic Ice Sheet (EAIS) and West Antarctic Ice Sheet (WAIS) but the processes controlling their in…