Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/150624
Share/Export:
logo share SHARE BASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE

Invite to open peer review
DC FieldValueLanguage
dc.contributor.authorAndrés, Juvenales_ES
dc.contributor.authorAlcalde, Juanes_ES
dc.contributor.authorAyarza, P.es_ES
dc.contributor.authorSaura, Eduardes_ES
dc.contributor.authorMarzán, Ignacioes_ES
dc.contributor.authorMartí, Davides_ES
dc.contributor.authorMartínez-Catalán, J. R.es_ES
dc.contributor.authorCarbonell, Ramónes_ES
dc.contributor.authorPérez-Estaún, Andréses_ES
dc.contributor.authorGarcía-Lobón, J.L.es_ES
dc.contributor.authorRubio Sánchez-Aguililla, Félix Manueles_ES
dc.date.accessioned2017-05-30T07:59:26Z-
dc.date.available2017-05-30T07:59:26Z-
dc.date.issued2016-06-28-
dc.identifier.citation9a Asamblea Hispano Portuguesa de Geodesia y Geofísica: (2016)es_ES
dc.identifier.urihttp://hdl.handle.net/10261/150624-
dc.description.abstractHontomín hosts the first Spanish CO2 storage research plant. The geophysical characterisation of the site included the acquisition of a 36 km2 3D seismic and a 16 km2 3D microgravimetric datasets. The integration of these data is here used to: (1) reproduce the deep structure and topography of the basement; (2) quantify the thickness of the Triassic Keuper evaporites, located between the sedimentary succession and the metamorphic basement; and (3) establish relationships between the faults interpreted in the seismic data and those inferred from the gravimetric data in the basement. The geometry of the sedimentary succession and structures interpreted from the seismic volume were used to constrain the inversion of the microgravity data: i.e. their gravimetric signature was calculated and then removed it from the Bouguer Anomaly. The top of the basement geometry was used, along that of the top of the Triassic Keuper, to calculate the salt thickness. The basement structure is characterized by a half-graben, thick-skinned setting filled with thick Keuper evaporites (up to 2000 m thick) forming an extensional forced fold. The two datasets identified two main fault systems compartmentalizing the structural domain into three differentiated blocks: the Central, South and East blocks. Furthermore, another inferred basement fault has been proposed to accommodate the thickening of the Triassic Keuper salts towards the NW of the area. These faults have been interpreted to be reactivated normal faults that led to the development of the Hontomín dome-
dc.relation.isversionofPublisher's version-
dc.rightsclosedAccess-
dc.titleCaracterización conjunta del basamento en Hontomín (España) empleando datos sísmicos y microgravimétricoses_ES
dc.typecomunicación de congresoes_ES
dc.date.updated2017-05-30T07:59:26Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066spa-
dc.relation.csices_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_5794es_ES
item.grantfulltextnone-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.openairetypecomunicación de congreso-
Appears in Collections:(Geo3Bcn) Comunicaciones congresos
(IGME) Comunicaciones congresos
Files in This Item:
File Description SizeFormat
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
View/Open
Show simple item record

CORE Recommender

Page view(s)

340
checked on May 21, 2024

Download(s)

37
checked on May 21, 2024

Google ScholarTM

Check


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