Sobre las deformaciones del paleozoico en el macizo del Desierto de las Palmas (Castellón)
DOI:
https://doi.org/10.3989/egeol.86426771Keywords:
Carboniferous, Hercynian tectonics, Iberian chain.Abstract
The Paleozoic deposits in the Desierto de las Palmas massif are turbidites whose probable age is lower Carboniferous. They registered a fírst deformation phase giving rise to very flattened recumbent folds, with associated slaty cleavage and NE-SW axes. Afterwards two phases of buckling folds with small flattening and crenulation cleavage are developed: the second one is ENE and the third one is N to NNW. A last superposed ESE crenulation is probably of Alpine age.
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