Campaign for the North is fighting for a devo-max Northern government with tax-raising powers.
We want a North that is governed by Northerners and for Northerners. Only then will we be able to step out of the shadow of London and have genuine control over our lives.
Campaign for the North is fighting for a devo-max Northern government with tax-raising powers.
We want a North that is governed by Northerners and for Northerners. Only then will we be able to step out of the shadow of London and have genuine control over our lives.
We at Flutura are helping Retail Energy Providers to realize value from their data.
These 7 nano apps for Retail Energy Providers helps them stay one step ahead of competition in a highly volatile market.
Flutura's Big Data Workshop - Flattening the JargonFlutura DS
Flutura's highly popular Big Data Workshop - Flattening the Jargon is back! Sessions starting December 1st.
For registrations and further queries, drop a mail to workshop@flutura.com.
Music : 'I dunno' by Grapes.
Recapitulation of some projects focused in 3D geological modelling.
- Surface based projects
- Seismic based projects
- Fault analysis based projects
- Facies modelling facies projects
- Well management based projects
3D Facies Modelling project using Petrel software. Msc Geology and Geophysics
Abstract
The Montserrat and Sant Llorenç del Munt fan-delta complexes were developed during the Eocene in the Ebro basin. The depositional stratigraphic record of these fan deltas has been described as a made up by a several transgressive and regressive composite sequences each made up by several fundamental sequences. Each sequence set is in turn composed by five main facies belts: proximal alluvial fan, distal alluvial fan, delta front, carbonates platforms and prodelta.
Using outcrop data from three composite sequences (Sant Vicenç, Vilomara and Manresa), a 3D facies model was built. The key sequential traces of the studied area georeferenced and digitalized on to photorealistic terrain models, were the hard data used as input to reconstruct the main surfaces, which are separating transgressive and regressive stacking patterns. Regarding the facies modelling has been achieved using a geostatistical algorithm in order to define the stacking trend and the interfingerings of adjacent facies belts, and five paleogeographyc maps to reproduce the paleogeometry of the facies belts within each system tract.
The final model has been checked, using a real cross section, and analysed in order to obtain information about the Delta Front facies which are the ones susceptible to be analogous of a reservoir. Attending to the results including eight probability maps of occurrence, the transgressive sequence set of Vilomara is the greatest accumulation of these facies explained by its agradational component.
We at Flutura are helping Retail Energy Providers to realize value from their data.
These 7 nano apps for Retail Energy Providers helps them stay one step ahead of competition in a highly volatile market.
Flutura's Big Data Workshop - Flattening the JargonFlutura DS
Flutura's highly popular Big Data Workshop - Flattening the Jargon is back! Sessions starting December 1st.
For registrations and further queries, drop a mail to workshop@flutura.com.
Music : 'I dunno' by Grapes.
Recapitulation of some projects focused in 3D geological modelling.
- Surface based projects
- Seismic based projects
- Fault analysis based projects
- Facies modelling facies projects
- Well management based projects
3D Facies Modelling project using Petrel software. Msc Geology and Geophysics
Abstract
The Montserrat and Sant Llorenç del Munt fan-delta complexes were developed during the Eocene in the Ebro basin. The depositional stratigraphic record of these fan deltas has been described as a made up by a several transgressive and regressive composite sequences each made up by several fundamental sequences. Each sequence set is in turn composed by five main facies belts: proximal alluvial fan, distal alluvial fan, delta front, carbonates platforms and prodelta.
Using outcrop data from three composite sequences (Sant Vicenç, Vilomara and Manresa), a 3D facies model was built. The key sequential traces of the studied area georeferenced and digitalized on to photorealistic terrain models, were the hard data used as input to reconstruct the main surfaces, which are separating transgressive and regressive stacking patterns. Regarding the facies modelling has been achieved using a geostatistical algorithm in order to define the stacking trend and the interfingerings of adjacent facies belts, and five paleogeographyc maps to reproduce the paleogeometry of the facies belts within each system tract.
The final model has been checked, using a real cross section, and analysed in order to obtain information about the Delta Front facies which are the ones susceptible to be analogous of a reservoir. Attending to the results including eight probability maps of occurrence, the transgressive sequence set of Vilomara is the greatest accumulation of these facies explained by its agradational component.