The Internal-External Betic Zone Boundary between Bullas and Zarzadilla de Totana is composed by the tectonic units of Peñarrubia-Castellar, El Francés Chaotic Complex, Las Canteras, Sierra de Ponce and Alquería, in the External Zone, and by the Morrón de Totana Unit belonging to the Malaguide Complex, in the Internal Zone. The structure of the Peñarrubia-Castellar Unit can be described as an FSF overturned synclinal whose hinge runs along the upper part of the Peñarrubia-Castellar mountain range.El presente trabajo ha sido realizado en el marco de los proyectos DGICYT: PB96-1430 y P96-0327 y del Grupo de Investigación RNM-208 de la Junta de Andalucía
Detailed work on the La Massana anticline reveals that it represents a structural unit bounded by la...
The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the th...
The Torcal de Antequera is situated in the Penibetic (part of the Betic External Zone) very near of ...
The Internal-External Betic Zone Boundary between Bullas and Zarzadilla de Totana is composed by the...
En las Béticas Occidentales, la Zona Transversal de Peñarrubia-Almargen (ZTPA) separa la Zona de Ci...
The position and kinematics of shear zones, which developed under different P-T conditions, lead to ...
n the NW of Sierra Tejeda (Spain) it is possible differentiate only two Alpujarride tectonic units, ...
El desarrollo de zonas transpresivas normalmente está relacionado con límites de placas de converge...
8 páginas, 4 figuras.[EN] Triassic materials belonging to the Malaguide Complex east of Cartagena ar...
In order to gain in the understanding of the evolution of the Betics, particularly in its Alpine fro...
Unraveling structural features related to different orogenic cycles is fundamental for a better unde...
La zona estudiada se sitúa en la zona cantábrica, que corresponde a la parte externa del orógeno her...
Between the Sierra de Ponce and the Peñarrubia-Castellar mountain ranges deposits of blocks-in-clay ...
A partir del levantamiento de un mapa geológico del borde occidental de la cuenca vasco cantábrica s...
Se describe la estratigrafía de la Unidad de la Peñarrubia al sur de Bullas.The Tertiary of the Peña...
Detailed work on the La Massana anticline reveals that it represents a structural unit bounded by la...
The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the th...
The Torcal de Antequera is situated in the Penibetic (part of the Betic External Zone) very near of ...
The Internal-External Betic Zone Boundary between Bullas and Zarzadilla de Totana is composed by the...
En las Béticas Occidentales, la Zona Transversal de Peñarrubia-Almargen (ZTPA) separa la Zona de Ci...
The position and kinematics of shear zones, which developed under different P-T conditions, lead to ...
n the NW of Sierra Tejeda (Spain) it is possible differentiate only two Alpujarride tectonic units, ...
El desarrollo de zonas transpresivas normalmente está relacionado con límites de placas de converge...
8 páginas, 4 figuras.[EN] Triassic materials belonging to the Malaguide Complex east of Cartagena ar...
In order to gain in the understanding of the evolution of the Betics, particularly in its Alpine fro...
Unraveling structural features related to different orogenic cycles is fundamental for a better unde...
La zona estudiada se sitúa en la zona cantábrica, que corresponde a la parte externa del orógeno her...
Between the Sierra de Ponce and the Peñarrubia-Castellar mountain ranges deposits of blocks-in-clay ...
A partir del levantamiento de un mapa geológico del borde occidental de la cuenca vasco cantábrica s...
Se describe la estratigrafía de la Unidad de la Peñarrubia al sur de Bullas.The Tertiary of the Peña...
Detailed work on the La Massana anticline reveals that it represents a structural unit bounded by la...
The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the th...
The Torcal de Antequera is situated in the Penibetic (part of the Betic External Zone) very near of ...