Search Results - "Ruiz‐Constán, A."

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    Reconstruction of the Exhumed Mantle Across the North Iberian Margin by Crustal‐Scale 3‐D Gravity Inversion and Geological Cross Section by Pedrera, A., García‐Senz, J., Ayala, C., RuizConstán, A., Rodríguez‐Fernández, L. R., Robador, A., González Menéndez, L.

    Published in Tectonics (Washington, D.C.) (01-12-2017)
    “…Recent models support the view that the Pyrenees were formed after the inversion of a previously highly extended continental crust that included exhumed upper…”
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    Journal Article
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    Deformation style and controlling geodynamic processes at the eastern Guadalquivir foreland basin (Southern Spain) by Marín‐Lechado, C., Pedrera, A., Peláez, J. A., RuizConstán, A., González‐Ramón, A., Henares, J.

    Published in Tectonics (Washington, D.C.) (01-06-2017)
    “…The tectonic structure of the Guadalquivir foreland basin becomes complex eastward evolving from a single depocenter to a compartmented basin. The deformation…”
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    Stress Field Evolution of the Southernmost Andean Cordillera From Paleostress Analysis (Argentine Tierra del Fuego) by Maestro, A., Ruano, P., Torres Carbonell, P., Bohoyo, F., Galindo‐Zaldívar, J., Pedrera, A., RuizConstán, A., González‐Castillo, L., Ibarra, P., López‐Martínez, J.

    Published in Tectonics (Washington, D.C.) (01-01-2019)
    “…The Argentine Tierra del Fuego comprises part of the roughly east‐west trending southern end of the Andean Cordillera intensely deformed since the Mesozoic…”
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    Seismic transpressive basement faults and monocline development in a foreland basin (Eastern Guadalquivir, SE Spain) by Pedrera, A., Ruiz-Constán, A., Marín-Lechado, C., Galindo-Zaldívar, J., González, A., Peláez, J. A.

    Published in Tectonics (Washington, D.C.) (01-12-2013)
    “…We examine the late Tortonian to present‐day deformation of an active seismic sector of the eastern Iberian foreland basement of the Betic Cordillera, in…”
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    Serpentinization-driven extension in the Ronda mantle slab (Betic Cordillera, S. Spain) by Pedrera, A., Galindo-Zaldívar, J., Acosta-Vigil, A., Azor, A., González-Menéndez, L., Rodríguez-Fernández, L.R., Ruiz-Constán, A.

    Published in Gondwana research (01-09-2016)
    “…We investigate the stress regimes acting during serpentinization and faulting of the largest known subcontinental lithospheric peridotite body, namely the…”
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    Structure of a complex carbonate aquifer by magnetic, gravity and TDEM prospecting in the Jaen area, Southern Spain by Ruiz-Constan, A, Pedrera, A, Martos-Rosillo, S, Galindo-Zaldivar, J, Ma, De Aguilar, J.P. Gonzalez

    Published in Geologica acta (01-09-2015)
    “…Knowledge of aquifer geometry is essential for efficient and sustainable groundwater management, particularly in carbonate aquifers due to uncertainties…”
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    Is the northwestern Betic Cordillera mountain front active in the context of the convergent Eurasia-Africa plate boundary? by Ruiz-Constán, A., Stich, D., Galindo-Zaldívar, J., Morales, J.

    Published in Terra nova (Oxford, England) (01-10-2009)
    “…The present relief of the Betic‐Rif Cordillera has been mainly developed since the Late Miocene in the context of the Eurasia–Africa NW–SE oblique convergence…”
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    Integrated geophysical methods for studying the karst system of Gruta de las Maravillas (Aracena, Southwest Spain) by Martínez-Moreno, F.J., Galindo-Zaldívar, J., Pedrera, A., Teixido, T., Ruano, P., Peña, J.A., González-Castillo, L., Ruiz-Constán, A., López-Chicano, M., Martín-Rosales, W.

    Published in Journal of applied geophysics (01-08-2014)
    “…In this study we contrast the results of different geophysical methods in order to describe the karst system surrounding of the Gruta de las Maravillas cave…”
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    Study of Schumann resonances based on magnetotelluric records from the western Mediterranean and Antarctica by Toledo-Redondo, S., Salinas, A., Portí, J., Morente, J. A., Fornieles, J., Méndez, A., Galindo-Zaldívar, J., Pedrera, A., Ruiz-Constán, A., Anahnah, F.

    “…Eight independent magnetotelluric (MT) campaigns, carried out in the western Mediterranean area and Antarctica, have been analyzed with the aim of extracting…”
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    Geomagnetism, Paleomagnetism and Electromagnetism Perspectives on Integrated, Coordinated, Open, Networked (ICON) Science by Ayala, C., Beamud, E., Huebert, J., Jones, S. A., Kumar, A., Miller, S. R., Moorkamp, M., Pueyo, E. L., RuizConstan, A., Schamuells, N., Sur, D., Tauxe, L., Hinsbergen, D. J. J.

    Published in Earth and space science (Hoboken, N.J.) (01-06-2022)
    “…This article is composed of three independent commentaries about the state of Integrated, Coordinated, Open, Networked (ICON) principles (Goldman et al., 2021,…”
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    Is there an active subduction beneath the Gibraltar orogenic arc? Constraints from Pliocene to present-day stress field by Pedrera, A., Ruiz-Constán, A., Galindo-Zaldívar, J., Chalouan, A., Sanz de Galdeano, C., Marín-Lechado, C., Ruano, P., Benmakhlouf, M., Akil, M., López-Garrido, A.C., Chabli, A., Ahmamou, M., González-Castillo, Lourdes

    Published in Journal of geodynamics (01-08-2011)
    “…► We provide the Pliocene and Quaternary stress map of the Gibraltar orogenic arc. ► The NW-SE push between Eurasia and Africa explain most of the observed S…”
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    Basin evolution associated to curved thrusts: The Prerif Ridges in the Volubilis area (Rif Cordillera, Morocco) by Roldán, F.J., Galindo-Zaldívar, J., Ruano, P., Chalouan, A., Pedrera, A., Ahmamou, M., Ruiz-Constán, A., Sanz de Galdeano, C., Benmakhlouf, M., López-Garrido, A.C., Anahnah, F., González-Castillo, L.

    Published in Journal of geodynamics (01-07-2014)
    “…The Volubilis Basin is located between two structural arcs formed by the Prerif Ridges that developed during and after sedimentation. The arcs correspond with…”
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    Gravity anomalies and orthogonal box fold development on heterogeneous basement in the Neogene Ronda Depression (Western Betic Cordillera) by Ruiz-Constán, A., Galindo-Zaldívar, J., Pedrera, A., de Galdeano, C. Sanz

    Published in Journal of geodynamics (01-04-2009)
    “…The Ronda Depression constitutes a Neogene intramontane basin located in the external zones of the Western Betic Cordillera. Major deformation structures…”
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