Add to ORKGThe purpose of this project is to define the modern subsurface temperature field of the central North Sea, and to develop a phenomenological explanation based on conduction and fluid-advective processes. The source of subsurface information is corrected bottom-hole temperatures (BHTs) from thirty wells located within the Central Graben and its flanking areas. Temperature-depth patterns reveal considerable variability (24.6 to 44.
The thermal history and maturation potential of the central Scotian Slope is constrained using a com...
The Lost City hydrothermal field (LCHF) is hosted in serpentinite at the crest of the Atlantis Massi...
A rapidly growing demand for improved understanding of the Dutch subsurface exists because of the ne...
The purpose of this project is to define the modern subsurface temperature field of the central Nort...
Extraordinary 3D seismic data from the Central Offshore Platform (Southern North Sea), complemented ...
The Horn Graben is a relatively under explored part of the Danish North Sea. Although extensive expl...
This paper integrates interpretations of modern long-offset seismic datasets with potential field an...
Zones of above average subsurface temperatures have been noted in certain areas of the Gulf Coast ba...
Understanding the subsurface dynamics of the world’s oceans has become more important over time due ...
The purpose of this study is to investigate the structure of the Viking Graben and adjacent areas u...
Rudkiewicz Jean-Luc, Vear Alwyn, Düppenbecker Stephan, Brigaud Frédéric. Mechanisms for high pressur...
The North Sea is a marginal, epeirogenic sea lying in an intra-plate setting on the NW European con...
International audienceIn the Provence basin, south-eastern France, more than 230 Bottom Hole Tempera...
In this thesis, four fluid flow systems are studied in terms of their development, venting activity,...
In the present paper it is shown how profiles consisting of closely spaced (≤10 m) temperature measu...
The thermal history and maturation potential of the central Scotian Slope is constrained using a com...
The Lost City hydrothermal field (LCHF) is hosted in serpentinite at the crest of the Atlantis Massi...
A rapidly growing demand for improved understanding of the Dutch subsurface exists because of the ne...
The purpose of this project is to define the modern subsurface temperature field of the central Nort...
Extraordinary 3D seismic data from the Central Offshore Platform (Southern North Sea), complemented ...
The Horn Graben is a relatively under explored part of the Danish North Sea. Although extensive expl...
This paper integrates interpretations of modern long-offset seismic datasets with potential field an...
Zones of above average subsurface temperatures have been noted in certain areas of the Gulf Coast ba...
Understanding the subsurface dynamics of the world’s oceans has become more important over time due ...
The purpose of this study is to investigate the structure of the Viking Graben and adjacent areas u...
Rudkiewicz Jean-Luc, Vear Alwyn, Düppenbecker Stephan, Brigaud Frédéric. Mechanisms for high pressur...
The North Sea is a marginal, epeirogenic sea lying in an intra-plate setting on the NW European con...
International audienceIn the Provence basin, south-eastern France, more than 230 Bottom Hole Tempera...
In this thesis, four fluid flow systems are studied in terms of their development, venting activity,...
In the present paper it is shown how profiles consisting of closely spaced (≤10 m) temperature measu...
The thermal history and maturation potential of the central Scotian Slope is constrained using a com...
The Lost City hydrothermal field (LCHF) is hosted in serpentinite at the crest of the Atlantis Massi...
A rapidly growing demand for improved understanding of the Dutch subsurface exists because of the ne...