The geodynamic evolution of the Internal Zone of the Betic Cordilleras (south‐east Spain): a model based on structural analysis and geothermobarometry

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Abstract
The Internal Zone of the Betic Cordilleras consists of several superimposed major thrust sheets with different P‐T‐t evolutions. On the basis of an integrated field, microscopic and laboratory study, the tectono‐metamorphic history of the Mulhacen Complex and Almanzora Unit has been reconstructed in detail. The Mulhacen Complex has been affected by at least five phases of penetrative deformation, which have been labelled Dx‐1, Dx, Dx+1, Dx+2 and Dx+3. Dx‐1, and Dx are related to continent‐continent collision, which is indicated by high pressure‐low temperature (HP/LT) and subsequent intermediate P/T metamorphic conditions. Dx+1 is related to crustal thinning and heterogeneous extension. During this event the Almanzora Unit was juxtaposed against the Mulhacen Complex. This phase was succeeded by the establishment of low pressure‐high temperature (LP/HT) conditions and at least two phases of folding and overthrusting. The Almanzora Unit shows a comparable tectono‐metamorphic evolution post Dx+1. However, the P/T conditions prior to Dx+1 indicate a higher crustal position with respect to the Mulhacen Complex during the collisional event.