Zobrazeno 1 - 4
of 4
pro vyhledávání: '"M. C. Osácar"'
Publikováno v:
Journal of Palaeogeography, Vol 8, Iss 1, Pp 1-20 (2019)
Abstract Textural and stable isotopic features of two middle Pleistocene fluvial stromatolite profiles are compared to a recent stromatolite, both formed in the River Piedra system (NE Spain), to test the reliability of climatic, hydrologic and depos
Externí odkaz:
https://doaj.org/article/70ba1bc2da2b4de4a96796b805a10280
Publikováno v:
Estudios Geologicos, Vol 70, Iss 2, Pp e021-e021 (2014)
Durante un año se han monitorizado las cuevas de La Paz y La Viña en el Sistema de Cuevas de Ortigosa de Cameros (NE de la Península Ibérica) para rastrear la señal isotópica del oxígeno desde la lluvia a la calcita espeleotémica, y así valo
Externí odkaz:
https://doaj.org/article/aa52684531f14b5886d4cdd806c2fdb3
Autor:
Juan José Villalaín, Luca Aldega, Teresa Román-Berdiel, Chiara Invernizzi, Belén Oliva-Urcia, Cristina García-Lasanta, Sveva Corrado, Chiara Caricchi, M. C. Osácar, Antonio M. Casas-Sainz
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
instname
Thrusting at shallow depths often precludes analysis by means of structural indicators effective in other geological contexts (e.g., mylonites, sheath folds, shear bands). In this paper, a combination of techniques (including structural analysis, mag
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