Exploration in a mature basin requires a detailed classification and standardisation of rock stratigraphy to adequately comprehend the depositional history and prospect architecture. The pre-Quaternary Stratigraphic Nomenclature of the Netherlands compiled by Van Adrichem Boogaert &Kouwe in 1993 provided a consistent framework for use by the Dutch geological community. Over the past twenty years, new biostratigraphic techniques and continued exploration in the Netherlands have provided additional stratigraphic information. Based on this information the Late Jurassic lithostratigraphy in particular, shows significant inaccuracies. The Callovian-Ryazanian strata from the northern offshore of the Netherlands’ territorial waters, termed the Cen...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
Due to the nature of the depositional environment and most importantly the lack of (bio) stratigraph...
Middle Jurassic - Early Cretaceous strata are a target for oil and gas exploration in the Dutch offs...
A revised Upper Cenozoic stratigraphic framework of the Dutch sector of the North Sea Basin is prese...
A revised Upper Cenozoic stratigraphic framework of the Dutch sector of the North Sea Basin is prese...
The classification of rocks and sediments may be based on many types of stratigraphy; e.g. litho-, b...
In the Netherlands North Sea area, the Chalk Group has thus far been subdivided into the Cenomanian ...
In the Netherlands North Sea area, the Chalk Group has thus far been subdivided into the Cenomanian ...
Jurassic shallow marine to non-marine depositional sequences are among the most important economic t...
Jurassic shallow marine to non-marine depositional sequences are among the most important economic t...
A recent revision of the lithostratigraphy of the Netherlands has triggered an extensive re-eval-uat...
3-D seismic survey data from the Central Graben of the Dutch North Sea has been interpreted applying...
A sequence stratigraphic framework is established for the Jurassic of the Danish Central Graben base...
Old borehole descriptions, modern lithostratigraphical classification and geostatistics have been co...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
Due to the nature of the depositional environment and most importantly the lack of (bio) stratigraph...
Middle Jurassic - Early Cretaceous strata are a target for oil and gas exploration in the Dutch offs...
A revised Upper Cenozoic stratigraphic framework of the Dutch sector of the North Sea Basin is prese...
A revised Upper Cenozoic stratigraphic framework of the Dutch sector of the North Sea Basin is prese...
The classification of rocks and sediments may be based on many types of stratigraphy; e.g. litho-, b...
In the Netherlands North Sea area, the Chalk Group has thus far been subdivided into the Cenomanian ...
In the Netherlands North Sea area, the Chalk Group has thus far been subdivided into the Cenomanian ...
Jurassic shallow marine to non-marine depositional sequences are among the most important economic t...
Jurassic shallow marine to non-marine depositional sequences are among the most important economic t...
A recent revision of the lithostratigraphy of the Netherlands has triggered an extensive re-eval-uat...
3-D seismic survey data from the Central Graben of the Dutch North Sea has been interpreted applying...
A sequence stratigraphic framework is established for the Jurassic of the Danish Central Graben base...
Old borehole descriptions, modern lithostratigraphical classification and geostatistics have been co...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
The northern Dutch offshore is an area that has seen less hydrocarbon exploration activity than othe...
Due to the nature of the depositional environment and most importantly the lack of (bio) stratigraph...