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• W2000920618 abstract "The Internal Zone of the Betic Cordilleras offers a unique opportunity to study the dynamics of lithospheric processes at mid crustal levels, which controlled the formation and evolution of the southeastern margin of Iberia. In this paper we present the result of two-dimensional numerical modelling of P-T-t paths related to latest Oligocene and Early Miocene extension and inversion in the Betic Zone. The ages of P-T-t loops are constrained by an extensive data set of geothermo-barometric and geochronological data, including 40Ar/39Ar laser probe data. We investigate the thermo-mechanical evolution of the Betic Zone using numerical models for simple shear, pure shear and combined shear. The Wernicke simple shear model fails to explain the observed temperatures in excess of 500°C and is not consistent with the occurrence of intrusions of ultramafic rocks in the western Betics. However, the delaminated simple shear model with low-angle faults located only at lower crustal levels, is found to be consistent with the P-T-t data. After a heating phase, associated with a finite extension of 80 km, rapid cooling occurred reflecting inversion of the extensional structure by NW-SE to N-S directed compression. Palaeo-rheological models for the latest Oligocene-Early Miocene times demonstrate the important role of the detachments produced during crustal extension for the dynamics of the subsequent inversion phase. The modelling strongly suggest that inversion locked after 60 km of finite convergence. After locking of the inversion, overthrusting in a northward direction occurred, which is compensated by pure shear deformation in the lower crust in the southeastern part of the Betic Zone." @default.
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• W2000920618 date "1992-03-01" @default.
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• W2000920618 title "Two-dimensional P-T-t modelling and the dynamics of extension and inversion in the Betic Zone (SE Spain)" @default.
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• W2000920618 doi "https://doi.org/10.1016/0040-1951(92)90229-y" @default.
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