Timing and structural evolution in the limb of an orocline: The Pisuerga-Carri贸n Unit (southern limb of the Cantabrian Orocline, NW Spain)
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文摘

Joint analysis in unconformity bounded strata show 40° of rotation.

Oroclinal buckling of Variscan belt started at Mychkovian.

The limb of the orocline underwent out-of-sequence thrusted.

Syn-orocline rocks deformed passively due to reactivation of former structures.

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