Salt tectonics structures and their associated sediments are classic targets for hydrocarbon exploration.
Fracture analysis and architecture of carbonate depositional systems
Dynamic stratigraphy, facies and architecture of fluvio-deltaic and coastal depositional systems
Fracture analysis and architecture of carbonate depositional systems
Appraisal and development of fractured carbonate reservoirs remains a significant challenge because of the generally high degree of heterogeneity i
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Dynamic stratigraphy, facies and architecture of fluvio-deltaic and coastal depositional systems
Appraisal and development of clastic reservoirs rely on sandbody geometries and porosity. In addition, most clastic reservoirs are affected by natu
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3-day field trip plus 1-day lectures
Salt tectonics structures and their associated sediments are classic targets for hydrocarbon exploration. Recently, the south-central Pyrenees are
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Facies, architecture and depositional systems
Fracture analysis and facies of Palaeozoic rocks and granites
Extensional to compressional tectonics and related sedimentation
Davinia completed her doctorate at the Universidad Complutense of Madrid where she helps with the teaching of courses such as ‘Perforation and core description’, ‘GIS and remote sensing’ and ‘Sedimentary environments’. She researches on the sedimentology and ichnology of marginal-marine environments and collaborates with the Research Group of Ichnology at the University of Saskatchewan.
Valentí is owner of an Andorran geological company, Igeotest Andorra. Projects have included Variscan mapping, near surface geophysical studies, hydrogeology in porous media and hard rocks, geotechnics, environmental impacts and natural hazards, geoarchaeology and glacial geology. Valentí also promotes science through the Maurice Chevalier Foundation. He’s our expert on the Variscan.
Geoplay Pyrenees Ltd has been carrying out field research and providing field courses for the petroleum industry since 1989.
View moreThe Pyrenees are an Alpine fold-thrust belt extending east to west along the north of the Iberian Peninsula and southern France, formed by the collision of plates during the Late Cretaceous–early Miocene.
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