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Microestructuras, luminiscencia y geoquímica en Crassostrea sp. de la Formación Zufía, Navarra (Albiense superior-Cenomaniense inferior). Parte IMicrostructures, luminescence and geochemical behaviour in Crassostrea sp. of the Zufia Formation, Navarra (Upper Albian-Lower Cenomanian). Part I
(2006)
Shells of the oyster Crassostrea sp. from the Zufia Formation, deposited in a strongly subsiding basin at the
end of the Albian, show the same microstructures than recent and fossil Crassostrea sp., deposited in other
less ...
Señales geoquímicas y micropaleontológicas como marcadores de eventos paleoceanográficos en el Santoniense del Arco VascoGeochemical and micropalaeontologic signals as palaeoceanographic event markers from the Santonian of the Basque Arc
(Sociedad Geológica de España, 2001)
Comparative study of micropalaeontologic (planktonic and benthic foraminifers) and isotopic (8,80 and 5'3C values from inoceramids and whole rock) data from the Santonian of the Barrika section (Basque Arc, northern Spain) ...
Modificaciones diagenéticas en la microestructura de los inocerámidos (Bivalvia) de la Formación de Plentzia (Santóniense, Arco Vasco)Diagenetic modifications from microstructure of inoceramid shells (Bivalvia) of the Plentzia Formation (Santonian, Basque Arc)
(Sociedad Geológica de España, 2001)
noceramid shells, from the Santonian of the Basque Arc, have been tested to determine the preservation of their original prismatic microstructure formed by low magnesium calcite (LMC). Petrography and cathodoluminescence ...
Mineralogía de arcillas y diagénesis en la Formación de Quintanaloma (Cretácico Superior, Norte de Burgos, España)Clay mineralogy and diagenesis in the Quintanaloma Formation sediments (Upper Cretaceous, Northern Burgos, Spain)
(Sociedad Geológica de España, 2003)
The preliminary results of mineralogical analysis of 28 inner platform carbonate samples taken from the Quintanaloma Formation sediments (Upper Campanian-Lower Maastrichtian) at the Credilla de Sedano section (northern ...
Período vital y ciclos de crecimiento en Praeradiolites ciryi e Hippurites quintanalomensis (Hippuritacea, Bivalvia, Cretácico Superior de Gredilla de Sedano, Norte de Burgos, España)Life-span and growth cycles in Praeradiolites ciryi and Hippurites quintanalomensis (Hippuritacea, Bivalvia, Upper Cretaceous of Gredilla de Sedano, Northern Burgos, Spain)
(Sociedad Geológica de España, 2003)
Several specimens of Praeradiolites ciryi FLOQUET (1991) and Hippurites quintanalomensis FLOQUET (1991), taken from the Quintanaloma Formation sediments (Upper Campanian-Lower Maastrichtian) at Gredilla de Sedano section ...
Luminiscencia frente a quimismo elemental en inocerámidos (Bivalvia) de facies profunda (Formación de Plentzia, Santóniense del Arco Vasco). (Parte I)Luminescence against elemental chemistry from deep facies inoceramids (Bivalvia) (Plentzia Formation, Santonian of the Basque Arc). (Part I)
(Sociedad Geológica de España, 2003)
Inoceramid shells (four individuals) from deep facies sediments of the Plentzia Formation) (Santonian,
Basque Arc) have been analysed to determine their elemental chemistry (Mg2*, Sr2*, Na+, Ba2*, Fe2* and Mn2*) using ...
Geoquímica microestructural en Praeradiolites ciryi (Hippuritacea, Bivalvia, Cretácico Superior de Gredilla de Sedaño, Norte de Burgos, España)Microstructural geochemistry of Praeradiolites ciryi (Hippuritacea, Bivalvia, Upper Cretaceous of Gredilla de Sedano, Northern Burgos, Spain)
(Sociedad Geológica de España, 2003)
The detailed geochemical evolution along two transects of the shell of one specimen of Praeradiolites ciryi is examined along annual, seasonal and fortnightly («doublet») sclerochronological records. The analyzed specimen ...
Catodoluminiscencia y diagénesis en conchas de rudistas (Bivalvia) del Cretácico Superior de Gredilla de Sedaño (Norte de Burgos, España)Cathodoluminescence and diagenesis in rudist shells (Bivalvia) from the Upper Cretaceous of Gredilla de Sedaño (Northern Burgos, Spain)
(Sociedad Geológica de España, 2002)
The Quintanaloma Fm (Campanian-Maastrichtian) was deposited in a shallow marine environment and contains a lot of rudist shells (Hippuritidae and Radiolitidae), some of them in life position. From a diagenetic point of ...
Inocerámidos y sedimento carbonatado (Maastrichtiense inferior, Arco Vasco): Comportamiento de la relación 180/160 y 13C/12C durante la diagénesis. (Parte II)Inoceramids and carbonate sediment (lower Maastrichtian, Basque Arc): Behaviour of the 180/,(0 and 73C/12C ratios during diagenesis. (Part II)
(Sociedad Geológica de España, 2001)
Oxygen and carbon isotopic analysis have been carried out on whole rock and inoceramid shell samples from deep-sea carbonate sediments at Sopelana II, Sopelana I and Zumaya sections (Basque Arc). The analytical results ...
Luminiscencia frente a quimismo elemental en inocerámidos (Bivalvía) de facies somera (Secciones de Isla de Castro y Villamartín, Santoniense de la Cuenca Vasco-Cantábrica). (Parte II)Luminescence against elemental chemistry from shallow facies inoceramids (Bivalvia) (Isla de Castro and Villamartín Sections, Santonian of the Basque-Cantabrian Basin). (Part II)
(Sociedad Geológica de España, 2003)
The luminescent behaviour and trace element contents (Mg2*, Sr2+, Na+, Ba2+, Fe2+ and Mn2+), for a total of 798 analysed spots distributed in five transects, have been determined in the inoceramid shells (three individuals) ...