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The evolution of western Scandinavian topography: a review of Neogene uplift versus the ICE (isostasy–climate–erosion) hypothesis
Tectonics and erosion are the driving forces in the evolution of mountain belts, but the
identification of their relative contributions remains a fundamental scientific problem in …
identification of their relative contributions remains a fundamental scientific problem in …
Cenozoic uplift and subsidence in the North Atlantic region: Geological evidence revisited
The topographic evolution of the “passive” margins of the North Atlantic during the last 65
Myr is the subject of extensive debate due to inherent limitations of the geological …
Myr is the subject of extensive debate due to inherent limitations of the geological …
Fluid flow features in hydrocarbon plumbing systems: What do they tell us about the basin evolution?
Fluid flow features such as sandstone intrusions, mud volcano systems and pockmarks
represent well-known geological structures generated due to flow of fluids in the subsurface …
represent well-known geological structures generated due to flow of fluids in the subsurface …
A revised correlation of Tertiary rocks in the British Isles and adjacent areas of NW Europe
C King - 2016 - books.google.com
This Special Report comprehensively describes the stratigraphy and correlation of the
Tertiary (Paleogene–Neogene) rocks of NW Europe and the adjacent Atlantic Ocean and is …
Tertiary (Paleogene–Neogene) rocks of NW Europe and the adjacent Atlantic Ocean and is …
Morphology and distribution of Oligocene and Miocene pockmarks in the Danish North Sea–implications for bottom current activity and fluid migration
This study gives the first description of 33 mid‐Oligocene and 646 late Miocene pockmarks
mapped in the Danish part of the central North Sea. The pockmarks are all highly elongated …
mapped in the Danish part of the central North Sea. The pockmarks are all highly elongated …
[HTML][HTML] Morphology, sedimentary infill and depositional environments of the Early Quaternary North Sea Basin (56–62 N)
Abstract The North Sea Basin has been subsiding during the Quaternary and contains
hundreds of metres of fill. Seismic surveys (170 000 km 2) provide new evidence on Early …
hundreds of metres of fill. Seismic surveys (170 000 km 2) provide new evidence on Early …
The evolution of the Dogger Bank, North Sea: A complex history of terrestrial, glacial and marine environmental change
CJ Cotterill, E Phillips, L James, CF Forsberg… - Quaternary Science …, 2017 - Elsevier
This paper presents a summary of the results of a detailed multidisciplinary study of the near
surface geology of the Dogger Bank in the southern central North Sea, forming part of a site …
surface geology of the Dogger Bank in the southern central North Sea, forming part of a site …
Morphology and pattern of Quaternary sedimentation in the North Sea Basin (52–62 N)
Abstract The Quaternary North Sea Basin, which extends from northwest mainland Europe
in the south (52° N) to the Norwegian Sea in the north (62° N), contains a thick (up to 1 km) …
in the south (52° N) to the Norwegian Sea in the north (62° N), contains a thick (up to 1 km) …
[HTML][HTML] Glacially induced faulting along the NW segment of the Sorgenfrei-Tornquist Zone, northern Denmark: Implications for neotectonics and Lateglacial fault …
Abstract The Sorgenfrei-Tornquist Zone (STZ) is the northwestern segment of the Tornquist
Zone and extends from Bornholm across the Baltic Sea and northern Denmark into the North …
Zone and extends from Bornholm across the Baltic Sea and northern Denmark into the North …
[HTML][HTML] Organic petrographic and geochemical insights into organic matter derived from land plants and marine algae in the Lark Formation, Danish North Sea
Climatic fluctuations from the Eocene to the Miocene highlight the importance of
investigating the paleoenvironment of the latest Eocene to the Middle Miocene Lark …
investigating the paleoenvironment of the latest Eocene to the Middle Miocene Lark …