Search Results - "Booth‐Rea, G."
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Late Miocene Extensional Collapse of Northern Tunisia
Published in Tectonics (Washington, D.C.) (01-06-2018)“…Two orthogonal extensional systems produced the extensional collapse of the Tell and Atlas thrust belts in northern Tunisia during the Late Miocene to Pliocene…”
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Metamorphic Domes in Northern Tunisia: Exhuming the Roots of Nappe Belts by Widespread Post‐Subduction Delamination in the Western Mediterranean
Published in Tectonics (Washington, D.C.) (01-06-2023)“…Cenozoic extension in the Western Mediterranean has been related to the dynamics of back‐arc domains. Although, in most of its orogenic belts extension…”
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Differentiating geology and tectonics using a spatial autocorrelation technique for the hypsometric integral
Published in Journal of Geophysical Research - Earth Surface (01-06-2009)“…Hypsometry is thought to be sensitive to tectonic uplift rates and lithology differences. In this study we calculated hypsometric integrals (HIs) using as…”
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Heterogeneous extension and the role of transfer faults in the development of the southeastern Betic basins (SE Spain)
Published in Tectonics (Washington, D.C.) (01-12-2014)“…Large strike‐slip faults in the eastern Betics are interpreted to have developed in a transcurrent setting in response to 4–6 mm/yr of Africa‐Iberia NW‐SE…”
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Quaternary tectonic activity in NW Jordan: Insights for a new model of transpression–transtension along the southern Dead Sea Transform Fault
Published in Tectonophysics (14-12-2016)“…The Dead Sea Transform Fault (DSTF) constitutes the transform plate boundary between the African and Arabian plates. The southern part of this fault has been…”
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Metamorphism and kinematics of the early deformation in the Variscan suture of SW Iberia
Published in Journal of metamorphic geology (01-09-2012)“…The early (Devonian) collisional stage in SW Iberia has been investigated through the analysis of deformation in the Cubito‐Moura schists, the main lithology…”
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Arc-parallel vs back-arc extension in the Western Gibraltar arc: Is the Gibraltar forearc still active?
Published in Geologica acta (2012)“…Extremely tight arcs, framed within the Eurasia-Africa convergence region, developed during the Neogene on both sides of the western Mediterranean. A complex…”
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Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian passive margin: The Tanger-Ketama Unit (External Rif, northern Morocco)
Published in Geologica acta (01-09-2013)“…The distribution pattern of diagenetic conditions to very low-grade metamorphism in the eastern Rif has been determined based on a study of clay-mineral…”
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Contrasting structural and P-T evolution of tectonic units in the southeastern Betics: Key for understanding the exhumation of the Alboran Domain HP/LT crustal rocks (western Mediterranean)
Published in Tectonics (Washington, D.C.) (01-04-2005)“…Thermobarometry using mica‐chlorite local equilibria and structural analysis of three tectonic units of the Alpujarride complex in the southeastern Betics…”
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SwathProfiler and NProfiler: Two new ArcGIS Add-ins for the automatic extraction of swath and normalized river profiles
Published in Computers & geosciences (01-07-2017)Get full text
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Geomorphic analysis of the Sierra Cabrera, an active pop-up in the constrictional domain of conjugate strike-slip faults: The Palomares and Polopos fault zones (eastern Betics, SE Spain)
Published in Tectonophysics (10-12-2012)“…The NNE–SSW sinistral Palomares and the conjugate dextral WNW–ESE striking Polopos fault zones terminate in the Sierra Cabrera antiform. In order to test the…”
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Exhumation, doming and slab retreat in the Betic Cordillera (SE Spain): in situ 40Ar/39Ar ages and PTdt paths for the Nevado-Filabride complex
Published in Journal of metamorphic geology (01-06-2005)“…The combination of metamorphic petrology tools and in situ laser 40Ar/39Ar dating on phengite (linking time of growth, compositions and PT conditions) enables…”
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Exhumation, doming and slab retreat in the Betic Cordillera (SE Spain): in situ40Ar/39Ar ages and P-T-d-t paths for the Nevado-Filabride complex
Published in Journal of metamorphic geology (01-06-2005)“…The combination of metamorphic petrology tools and in situ laser 40Ar/39Ar dating on phengite (linking time of growth, compositions and P–T conditions) enables…”
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Stress analysis of NW Jordan: New episode of tectonic rejuvenation related to the Dead Sea transform fault
Published in Arabian journal of geosciences (01-04-2016)“…We performed a stress analysis based on fault-slip data for two of the main geological structures in NW Jordan; the Amman-Hallabat (AHF) and Shueib (SHF)…”
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Small-scale faulting, topographic steps and seismic ruptures in the Alhambra (Granada, southeast Spain
Published in Journal of quaternary science (01-03-2004)“…The Alhambra (14th century AD) in Granada (southeast Spain) is built at the summit of a Pliocene to Lower Pleistocene conglomeratic formation. Tens of…”
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Continental subduction, intracrustal shortening, and coeval upper-crustal extension: P-T evolution of subducted south Iberian paleomargin metapelites (Betics, SE Spain)
Published in Tectonophysics (16-11-2015)“…The Nevado–Filabride complex represents the basement and Permo-Triassic cover of the south Iberian passive margin, metamorphosed during Miocene continental…”
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Active tectonics and drainage evolution in the Tunisian Atlas driven by interaction between crustal shortening and mantle dynamics
Published in Geomorphology (Amsterdam, Netherlands) (15-02-2020)“…Active tectonics in North Africa are fundamentally driven by NW-SE directed slow convergence between the Nubia and Eurasia plates, leading to a region of…”
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Relief and drainage evolution during the exhumation of the Sierra Nevada (SE Spain): Is denudation keeping pace with uplift?
Published in Tectonophysics (16-11-2015)“…We have performed a geomorphic analysis of the Sierra Nevada, the highest range of the Betic Cordillera (SE Spain), with the aim to elucidate its late Miocene…”
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Active fault segmentation in Northern Tunisia
Published in Journal of structural geology (01-10-2020)“…Active shortening structures in Northern Tunisia have developed by tectonic inversion since the Pliocene, after Late Miocene extensional collapse of the whole…”
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