The Fortuna section has been studied in order to select a suitable section in Spain that could be a good candidate to define the Ypresian/Lutetian boundary stratotype. At present, this section is the most suitable, mainly because it is a complete marine section, well exposed and very rich in microfossils. A variation of mineralogical composition on the clays coincides with the most important change in planktonic foraminifera across the Y/L boundary. At this location, the data allowed us to infer a transgressive event associated with important hot and wet climatic changes that are the origin of an alteration and neoformation processes of clay mineral
El análisis de la composición mineralógica global de los sedimentos Lago-Mare y del Zancliense infe...
Lower Jurassic in the Betic Cordilleras (SE Spain). The six assemblages contain varying proportions ...
International audienceThe Late Messinian of the Sorbas Basin (Betic Cordillera, SE Spain) has been s...
with 6 figures Abstract. This integrated study across the Ypresian/Lutetian boundary in the Fortuna ...
This integrated study across the Ypresian/Lutetian boundary in the Fortuna Section (Spain) allowed u...
Séveral sections has been studied across the Murcia Region in arder to select a suitable section in ...
Marker events to define the stratotype for the base of the Lutetian Stage are poorly defined. To elu...
The Gorrondatxe beach section is part of a 2300 m thick lower Ypresian-upper Lutetian deep-water mar...
One of the Paleogene Stage boundaries still needing official definition is the Ypresian/Lutetain (Ea...
This work aims to study recent climatic oscillations and their influence on sedimentation in the Ria...
ABSTRACT: Benthic foraminifera were studied as part of an investigation of the Fortuna Section (Beti...
The clay mineral association of the Lorca basin (Murcia) is built by muscovite, chlorite (clinochlor...
A study of the rocks from the Miocene-Pliocene boundary at the Garrapancho ridge, in the southern se...
ABSTRACT: This study examines part of the thick palaeoweathering mantle that formed on the northern ...
The spatial and vertical distributions of six clay mineral assemblages were identified in the pelagi...
El análisis de la composición mineralógica global de los sedimentos Lago-Mare y del Zancliense infe...
Lower Jurassic in the Betic Cordilleras (SE Spain). The six assemblages contain varying proportions ...
International audienceThe Late Messinian of the Sorbas Basin (Betic Cordillera, SE Spain) has been s...
with 6 figures Abstract. This integrated study across the Ypresian/Lutetian boundary in the Fortuna ...
This integrated study across the Ypresian/Lutetian boundary in the Fortuna Section (Spain) allowed u...
Séveral sections has been studied across the Murcia Region in arder to select a suitable section in ...
Marker events to define the stratotype for the base of the Lutetian Stage are poorly defined. To elu...
The Gorrondatxe beach section is part of a 2300 m thick lower Ypresian-upper Lutetian deep-water mar...
One of the Paleogene Stage boundaries still needing official definition is the Ypresian/Lutetain (Ea...
This work aims to study recent climatic oscillations and their influence on sedimentation in the Ria...
ABSTRACT: Benthic foraminifera were studied as part of an investigation of the Fortuna Section (Beti...
The clay mineral association of the Lorca basin (Murcia) is built by muscovite, chlorite (clinochlor...
A study of the rocks from the Miocene-Pliocene boundary at the Garrapancho ridge, in the southern se...
ABSTRACT: This study examines part of the thick palaeoweathering mantle that formed on the northern ...
The spatial and vertical distributions of six clay mineral assemblages were identified in the pelagi...
El análisis de la composición mineralógica global de los sedimentos Lago-Mare y del Zancliense infe...
Lower Jurassic in the Betic Cordilleras (SE Spain). The six assemblages contain varying proportions ...
International audienceThe Late Messinian of the Sorbas Basin (Betic Cordillera, SE Spain) has been s...