The geological macrostructure of Alto Tajo is defined by several N150ºE 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: N60ºE compression; N150ºE compression (the main deformation phase). N-S compression, without important structures asociated and a last episode of radial extension.
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