Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Gabriela Fernández Viejo"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Cantabrian fault (CF) is a crustal-scale structure that cuts obliquely the western North Iberian Margin (NIM) for 160 km and continues onshore transecting the Cantabrian Mountains (CM) for another 150 km as the Ventaniella fault (VF). For most of
Externí odkaz:
https://doaj.org/article/7bfb6ddb02384b93b3ea5ba183fe6c2e
Autor:
Patricia Cadenas Martínez, J. Kim Welford, João C. Duarte, Gabriela Fernández-Viejo, Luis Somoza
The structure of Iberian Atlantic margins resulted from multiple Mesozoic rift events and subsequent contractional deformation occurring from the Upper Cretaceous to Cenozoic during the Alpine Orogeny. Along the southern Bay of Biscay, the North Iber
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4e216684111fe602261cae904f67392
https://doi.org/10.5194/egusphere-egu23-6654
https://doi.org/10.5194/egusphere-egu23-6654
Autor:
Javier Olona, Jorge Acevedo, Sergio Llana-Fúnez, Gabriela Fernández-Viejo, Carlos López-Fernández
Publikováno v:
Seismological Research Letters. 92:421-436
The upper-crustal anisotropy of the Cantabrian Mountains (North Spain) has been investigated using two independent but complementary methodologies: (a) shear-wave splitting and (b) ambient seismic noise interferometry. For this purpose, we have proce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::188f16872d427a3b3da9fc645a583258
https://doi.org/10.1785/0220200103
https://doi.org/10.1785/0220200103
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
5 pages, 3 figures, supplemental material https://doi.org/10.1130/G49341.1
Crustal roots are identified in collision chains worldwide. Frequently mirroring the summits of mountain systems, they elegantly encapsulate the concept of isostasy. The
Crustal roots are identified in collision chains worldwide. Frequently mirroring the summits of mountain systems, they elegantly encapsulate the concept of isostasy. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::67ab4627f4352fc5c25778f0928ec92f
http://hdl.handle.net/10261/258940
http://hdl.handle.net/10261/258940
Autor:
Jorge Acevedo, Carlos López-Fernández, Sergio Llana-Fúnez, Gabriela Fernández-Viejo, Diego Pérez-Millán, Javier Olona
Publikováno v:
Scopus
The cross-correlation of ambient noise records registered by seismic networks has proven to be a valuable tool to obtain new insights into the crustal structure at different scales. Based on 2 to 14 s period Rayleigh and Love dispersion data extracte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa2224434a127964848c976be629fc16
https://doi.org/10.5194/se-2021-116
https://doi.org/10.5194/se-2021-116
Autor:
Mario Ruiz, Sergio Llana-Fúnez, Gabriela Fernández-Viejo, Diego Pérez-Millán, Jorge Acevedo, Luis Pando, Jordi Diaz
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
EGU General Assembly 2021, vEGU21: Gather Online ,19–30 April 2021
The Variscan belt was formed as a consequence of the collision of two major continents, Laurasia and Gondwana, in the late Paleozoic. Nowadays, it constitutes the basement of t
The Variscan belt was formed as a consequence of the collision of two major continents, Laurasia and Gondwana, in the late Paleozoic. Nowadays, it constitutes the basement of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eebae14e9470effda9830673f661bf4a
https://doi.org/10.5194/egusphere-egu21-20
https://doi.org/10.5194/egusphere-egu21-20
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
The Cantabrian fault (CF) is a crustal-scale structure that cuts obliquely the western North Iberian Margin (NIM) for 160 km and continues onshore transecting the Cantabrian Mountains (CM) for another 150 km as the Ventaniella fault (VF). For most of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f1bfe07a93175b4a50aa28c0d637800
https://www.frontiersin.org/articles/10.3389/feart.2021.645061/full
https://www.frontiersin.org/articles/10.3389/feart.2021.645061/full
Crustal roots are a consequence of the contraction of continental masses during orogenesis identified in collisional chains worldwide. Frequently mirroring the summits of mountain systems, they portray the fundamental topic of isostasy. The northern
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d14f3fc10bee0c04f570558d2d74e3bf
https://doi.org/10.5194/egusphere-egu2020-13772
https://doi.org/10.5194/egusphere-egu2020-13772
In this work, we address the problem of the formation and reactivation of multi-stage rifting based on the study of the central North Iberian margin, located at the southern Bay of Biscay triangular oceanic domain. This magma-poor rifted margin regis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c39e0b1ffc6f8e7acb6ea8e916e72941
https://doi.org/10.5194/egusphere-egu2020-3964
https://doi.org/10.5194/egusphere-egu2020-3964