Cinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)
Loading...
Download
Official URL
Full text at PDC
Publication date
1994
Advisors (or tutors)
Editors
Journal Title
Journal ISSN
Volume Title
Publisher
Seminario de Estudos Galegos. Area de Xeoloxía e Minería ; Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
Citations
Exportar
Citation
Abstract
The geological macrostructure of Alto Tajo is defined by several N1500E dextral strike-slip faults with related secundary structures. The former set of faults together with others N-S sinistral strike-slip faults delimited areas in transtension and transpession. Four tectonic phases have been detected by means of microstructural analysis: N600E compression; N1500E compression (the main deformation phase). N-S compression, without important structures asociated and a last episode of radial extension.