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Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data

AutorAndrés, Juvenal ; Alcalde, Juan ; Ayarza, P.; Saura, Eduard ; Marzán, Ignacio; Martí, David ; Martínez Catalán, J. R.; Carbonell, Ramón ; Pérez-Estaún, Andrés ; García-Lobón, J.L.; Rubio, F.M.
Palabras clave3D seismics
sísmica 3D
Microgravimetría
geología estructural
Microgravity
basamento
basement
structural geology
Fecha de publicación12-sep-2016
EditorSociedad Geológica de España
CitaciónGeotemas 16: 523-526 (2016)
ResumenThe 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.
URIhttp://hdl.handle.net/10261/148209
Aparece en las colecciones: (ICTJA) Comunicaciones congresos
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