Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Óscar Pueyo Anchuela"'
Autor:
Jesús V. Picazo Millán, Fernando Pérez-Lambán, Javier Fanlo Loras, M. Marta Sampietro-Vattuone, José Luis Peña-Monné, Óscar Pueyo Anchuela, Andrés Pocoví Juan, Andoni Tarriño Vinagre
Publikováno v:
Munibe Antropologia-Arkeologia, Vol 74 (2023)
Presentamos un complejo minero dedicado a la extracción del sílex denominado Botorrita-Monegros, demandado en diferentes momentos de la Prehistoria. Para su documentación se programó una prospección a tres escalas: 1) prospección superficial in
Externí odkaz:
https://doaj.org/article/22c032b31eaa44e09df345c6bb5f691f
Autor:
Antonio María Casas Sáinz, Óscar Pueyo Anchuela, Javier Gracia Abadías, Andrés Pocoví Juan, Carlos Luis Liesa Carrera
Publikováno v:
International Journal of Speleology, Vol 46, Iss 2, Pp 237-249 (2017)
Zaguán. Repositorio Digital de la Universidad de Zaragoza
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Zaguán. Repositorio Digital de la Universidad de Zaragoza
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Evaluation of karst hazards benefits from the integration of different techniques, methodologies and approaches. Each one presents a different signature and is sensitive to certain indicators related to karst hazards. In some cases, detailed analysis
Publikováno v:
International Journal of Earth Sciences. 105:2221-2239
The Concud Fault is a ~14-km-long active fault that extends close to Teruel, a city with about 35,000 inhabitants in the Iberian Range (NE Spain). It shows evidence of recurrent activity during Late Pleistocene time, posing a significant seismic haza
Autor:
Pilar Diarte Blasco, Andrés Pocoví Juan, Carlos García Benito, Óscar Pueyo Anchuela, Antonio María Casas Sáinz
Publikováno v:
Archaeological Prospection. 23:105-123
The low contrast in physical properties of archaeological elements compared to the host soil is a common drawback in geophysical surveys applied to subtle archaeological sites because those contrasts are usually what are being measured by most instru
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
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instname
Karst hazards in the central Ebro Basin are related to subsidence and collapses owing to evaporitic rocks located several tens of metres below the surface. In this type of karst (mantle karst) cavities propagate upwards through a non-soluble rock, in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::598e207019a1da37ed406b5039ef98b0
http://zaguan.unizar.es/record/59205
http://zaguan.unizar.es/record/59205
Autor:
Andrés Pocoví Juan, Óscar Pueyo Anchuela, Antonio Pérez, María Asunción Soriano, Héctor Gil Garbi, Aránzazu Luzón
Publikováno v:
Journal of Applied Geophysics. 102:81-95
An integrated analysis was carried out in a selected quarry of the oldest terrace of the Ebro River, where a wide gravel unit is characterized by large-scale cross bedding outcrops. This unit has been interpreted as a lake with marginal deltas. Previ
Publikováno v:
Studia Geophysica et Geodaetica. 57:692-709
We analyse paramagnetic, ferrimagnetic and frequency-dependent susceptibility in the southern Pyrenees and northern Ebro basin. The analyzed rocks show a wide range of values for the three parameters within the different lithological groups. Sandston
Autor:
Antonio M. Casas-Sainz, Emilio L. Pueyo, Andrés Pocoví Juan, Óscar Pueyo Anchuela, Andrés Gil Imaz
Publikováno v:
Terra Nova. 25:307-314
Magnetic susceptibility in rocks is the sum of the contributions of different magnetic particles (paramagnetic, diamagnetic and ferromagnetic s.l.). These contributions can be measured at variable temperatures or at variable fields (hysteresis loops)
Publikováno v:
International Journal of Earth Sciences. 102:1131-1149
A combined sedimentological, shape-preferred orientation and anisotropy of magnetic susceptibility (AMS) analysis has been performed at the Arroyofrio Bed (Callovian–Oxfordian boundary level) in the locality of Moneva (Iberian Range, NE Spain). The
Publikováno v:
Comptes Rendus Geoscience. 343:11-19
Fine-grained sediments are generally better strain-markers in the outer part of orogenic belts and foreland basins because they are more prone to cleavage formation than coarse detrital rocks in diagenetic to very-low metamorphic environments. This a