In order to determine the structure of the Chalk in the London Basin, a combined cognitive and numerical approach to model construction was developed. A major difficultly in elucidating the structure of the Chalk in the London Basin is that the Chalk is largely unexposed. The project had to rely on subsurface data such as boreholes and site investigation reports. Although a high density of data was available problems with the distribution of data and its quality meant that, an approach based on a numerical interpolation between data points could not be used in this case. Therefore a methodology was developed that enabled the modeller to pick out areas of possible faulting and to achieve a geologically reasonable solution even in areas wher...
This report describes the geological modelling of the North Downs in Kent, between the River Medway ...
As a provider of geological advice to industry, academia and the public, the British Geological Surv...
Chalk is an important aquifer in England. Because of the highly permeable nature of the subsurface, ...
This paper will describe firstly the combined cognitive and geostatistical modelling methodology tha...
Many geological survey organisations have started delivering digital geological models as part of th...
This report describes the work undertaken to produce the London Chalk Model (LCM) within the catchme...
A fortuitous combination of events in the last 30 years has positioned the Chalk as the most eligibl...
AbstractMany geological survey organisations have started delivering digital geological models as pa...
A proliferation of 3D geological models has been created by the British Geological Survey (BGS) ove...
This report describes the rationale and procedure for the construction of a new high-resolution str...
Over the last decade many Geological Survey Organisations worldwide have begun to communicate their ...
Since the last Chalk symposium in 1989 in Brighton, our understanding of the UK Chalk has undergone ...
In recent years, with the improvement of computer processing power and the development of sophistica...
AbstractThe Chalk is a major aquifer, source of raw material for cement and agricultural lime, and a...
Adequate hydrogeological conceptualisation of structurally complex fractured aquifers requires the ...
This report describes the geological modelling of the North Downs in Kent, between the River Medway ...
As a provider of geological advice to industry, academia and the public, the British Geological Surv...
Chalk is an important aquifer in England. Because of the highly permeable nature of the subsurface, ...
This paper will describe firstly the combined cognitive and geostatistical modelling methodology tha...
Many geological survey organisations have started delivering digital geological models as part of th...
This report describes the work undertaken to produce the London Chalk Model (LCM) within the catchme...
A fortuitous combination of events in the last 30 years has positioned the Chalk as the most eligibl...
AbstractMany geological survey organisations have started delivering digital geological models as pa...
A proliferation of 3D geological models has been created by the British Geological Survey (BGS) ove...
This report describes the rationale and procedure for the construction of a new high-resolution str...
Over the last decade many Geological Survey Organisations worldwide have begun to communicate their ...
Since the last Chalk symposium in 1989 in Brighton, our understanding of the UK Chalk has undergone ...
In recent years, with the improvement of computer processing power and the development of sophistica...
AbstractThe Chalk is a major aquifer, source of raw material for cement and agricultural lime, and a...
Adequate hydrogeological conceptualisation of structurally complex fractured aquifers requires the ...
This report describes the geological modelling of the North Downs in Kent, between the River Medway ...
As a provider of geological advice to industry, academia and the public, the British Geological Surv...
Chalk is an important aquifer in England. Because of the highly permeable nature of the subsurface, ...