Zobrazeno 1 - 10
of 68
pro vyhledávání: '"Ó. Pueyo-Anchuela"'
Autor:
A. Peiro, J.L. Simón, L.E. Arlegui, L. Ezquerro, A.I. García-Lacosta, M.T. Lamelas, C.L. Liesa, A. Luzón, L. Martín-Bello, Ó. Pueyo-Anchuela, N. Russo
Publikováno v:
Tectonophysics. 828:229274
Autor:
V. Beolchini, Leonor Peña-Chocarro, Antonio M. Casas, Pilar Diarte-Blasco, A. Muñoz, Andrés Pocoví, Juan José Villalaín, Ó. Pueyo-Anchuela
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
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A detailed magnetic survey combined with the study of magnetic properties and spectral analysis in the Tusculum archaeological site (Alban Hills, Italy) indicates the existence of magnetic anomalies (total field and gradient, showing amplitudes up to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1272b93cded2dec5a0bff2be8267a6a
http://hdl.handle.net/10261/229573
http://hdl.handle.net/10261/229573
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
instname
The stability of embankment dams without an impermeable core depends on the characteristics of the face slab that prevents internal erosion, piping and eventual collapse of the structure. Under a Mediterranean climate, the impermeable asphaltic face
Publikováno v:
Marine and Petroleum Geology. 76:329-343
The well exposed outcrops of the upper Kimmeridgian shallow-marine carbonates at Jabaloyas (Iberian Chain, NE Spain) permit the evaluation of geophysical methods for the identification of sedimentary facies. Direct measurement of magnetic susceptibil
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
instname
The Quaternary Añavieja-Dévanos tufa system is located in the northern sector of the Iberian Chain. It has been previously tackled by means sedimentological studies focused on the available outcrops and some boreholes. They have permitted the propo
Autor:
Teresa Román-Berdiel, Cristina García-Lasanta, M. C. Osácar, A.M. Casas-Sainz, Chiara Invernizzi, A. Gil-Imaz, Esther Izquierdo-Llavall, Luca Aldega, Chiara Caricchi, M. Ansón, José L. Simón, Ó. Pueyo-Anchuela, Sveva Corrado
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2018, 730, pp.29-47. ⟨10.1016/j.tecto.2018.02.013⟩
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
Tectonophysics, Elsevier, 2018, 730, pp.29-47. ⟨10.1016/j.tecto.2018.02.013⟩
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
Anisotropy of magnetic susceptibility (AMS) has been applied to the study of shallow fault zones, although interpretation of the results requires establishing clear relationships between petrofabric and magnetic features, magnetic behaviour of fault
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::641348fd9217b5e6210d1f3d8ba98653
http://hdl.handle.net/11573/1131471
http://hdl.handle.net/11573/1131471
Autor:
Ó. Pueyo Anchuela, P. L. López Julián, J. Ramajo Cordero, Carlos L. Liesa, A. Pocoví Juan, J.A. Pérez Benedicto, A.M. Casas Sainz
Publikováno v:
Engineering Geology. 193:158-172
At mantle/cover evaporite karst settings, evidences of surficial subsidence are usually strongly dependent on geomechanical properties and spatial inhomogeneities within the cover series. In infrastructure assets, affected by karst processes, the eva
Publikováno v:
Engineering Geology. 184:29-42
Mantle karst environments can be analyzed by means of historical, geophysical and geomechanical approaches with the objectives of avoiding urban development in hazardous areas or to establish guidelines for foundation design. Nevertheless, geophysica
Publikováno v:
Environmental Earth Sciences. 76
Dispersion of pollutants from mining areas can result in risks to human health. The dynamic interaction of geological processes can generate complex situations that favor enrichment in toxic elements by sedimentary and diagenetic mechanisms. In order
Autor:
Jesús Galindo-Zaldívar, Inmaculada Gil-Peña, Ó. Pueyo Anchuela, J. Rey, Belén Oliva-Urcia, Ruth Soto, Jerónimo López-Martínez, Adolfo Maestro, A. Gil Imaz
Publikováno v:
Tectonophysics. 626:69-85
The analyses of recent volcanic systems can encounter limitations due to recent eruptions hiding part of the geological history, where the geomorphological expression can present non-univocal interpretations or where modern relief and abrupt cliffs c