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Exhumation of the Ronda peridotite and its crustal envelope: constraints from thermal modelling of a P-T-time array

Platt, J.P; Argles, T.W; Carter, A.; Kelley, S.P; Whitehouse, M.J and Lonergan, L. (2004). Exhumation of the Ronda peridotite and its crustal envelope: constraints from thermal modelling of a P-T-time array. Journal of the Geological Society, 160(5) pp. 655–676.

URL: http://www.ingentaconnect.com/content/geol/jgs/200...
DOI (Digital Object Identifier) Link: http://dx.doi.org/10.1144/0016-764902-108
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Abstract

The Ronda pendotite in the Bette Cordillera Of Southern Spain is a relic of the sub-orogenic lithospheric mantle that was exhumed during earliest Miocene time from about 66 km depth. Overlying crustal rocks show an apparently coherent metamorphic zonation front high-pressure granulite-facies rocks at the contact to unmetamorphosed rocks 5 kin higher in the structural sequence, indicating drastic tectonic thinning of the whole orogenic crust during exhumation. P-T paths from the peridotite and its crustal envelope indicate decompression with rising temperature to shallow depths. U-Pb ion microprobe dating of zircon, Ar/Ar dating of hornblende, Ar/Ar laserprobe dating of muscovite and biotite, and fission-track analysis of zircon and apatite reveal that cooling was extremely rapid in the interval 21.2-20.4 Ma. One-dimensional thermal modelling of the array of P-T-time paths indicates that an asthenospheric heat source at an initial depth of about 67.5 km is required to explain heating during exhumation, and that the main period of exhumation lasted 5 Ma, starting at around 25 Ma. Exhumation Must therefore have directly followed removal of most, but not all, of the lithospheric mantle beneath the Betic orogen, and was coeval with a period of late orogenic extension that profoundly modified the crustal structure and created the present-day Alboran Sea in the western Mediterranean.

Item Type: Journal Article
ISSN: 0016-7649
Keywords: Bette Cordillera; absolute age; exhumation; thermobarometry; extensional tectonics; peak metamorphic conditions; high-pressure metamorphism; Western Betic Cordilleras; Southern Spain; Alboran domain; S.E. Spain; Alpujarride complex; rapid exhumation; temperature metamorphism; continental lithosphere
Academic Unit/Department: Science > Environment, Earth and Ecosystems
Interdisciplinary Research Centre: Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)
eSTEeM
Item ID: 2110
Depositing User: Simon Kelley
Date Deposited: 05 Jun 2006
Last Modified: 05 Mar 2014 10:10
URI: http://oro.open.ac.uk/id/eprint/2110
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