English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/148209
Share/Impact:
Statistics
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorAndrés, Juvenal-
dc.contributor.authorAlcalde, Juan-
dc.contributor.authorAyarza, P.-
dc.contributor.authorSaura, Eduard-
dc.contributor.authorMarzán, Ignacio-
dc.contributor.authorMartí, David-
dc.contributor.authorMartínez Catalán, J. R.-
dc.contributor.authorCarbonell, Ramón-
dc.contributor.authorPérez-Estaún, Andrés-
dc.contributor.authorGarcía-Lobón, J.L.-
dc.contributor.authorRubio, F.M.-
dc.date.accessioned2017-04-10T10:41:11Z-
dc.date.available2017-04-10T10:41:11Z-
dc.date.issued2016-09-12-
dc.identifier.citationGeotemas 16: 523-526 (2016)-
dc.identifier.urihttp://hdl.handle.net/10261/148209-
dc.description.abstractThe structure of the Hontomín CO2 geological storage research facility has been addressed combining 3D seismic reflection data, borehole information and microgravity data. The integrated interpretation constrains the basement structural setting geometry and that of the sedimentary succession. The study unravels the deep structure and topography of the basement and quantifies the thickness of the Triassic Keuper evaporites. We describe a half-grabensetting filled with Keuper evaporites (up to 2000 m) forming an extensional forced fold. Three set of faults are identified with two main fault systems compartmentalizing the area into three differentiated blocks. These faults have been interpreted to be reactivated normal faults that have led to the formation of the Hontomín dome.-
dc.description.sponsorshipThe datasets in this work have been funded by Fundación Ciudad de la Energía (Spanish Government, www.ciuden.es) and by the European Union throughthe “European Energy Programme for Recovery” and the Compostilla OXYCFB300 project. Dr. Juan Alcalde is currently funded by NERC grant NE/M007251/1.-
dc.publisherSociedad Geológica de España-
dc.relation.isversionofPublisher's version-
dc.rightsopenAccess-
dc.subject3D seismics-
dc.subjectsísmica 3D-
dc.subjectMicrogravimetría-
dc.subjectgeología estructural-
dc.subjectMicrogravity-
dc.subjectbasamento-
dc.subjectbasement-
dc.subjectstructural geology-
dc.titleBasement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data-
dc.typecomunicación de congreso-
dc.date.updated2017-04-10T10:41:11Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.relation.csic-
Appears in Collections:(Geo3Bcn) Comunicaciones congresos
Files in This Item:
File Description SizeFormat 
Basement structure.pdf653,21 kBAdobe PDFThumbnail
View/Open
Show simple item record
 


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.