2026-06-08T09:32:28Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/525352023-08-25T12:41:04Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Gutiérrez Alonso, Gabriel
author
Fernández Suárez, Javier
author
Weil, Arlo B.
2023-06-20T12:47:37Z
2023-06-20T12:47:37Z
2004
1576-5172
https://hdl.handle.net/20.500.14352/52535
http://www.sociedadgeologica.es/publicaciones_geotemas.html
Late- to post-orogenic oroclinal bending in conjunction with thinning of the lithospheric mantle is potentially an important component of the waning stages of plate convergence in collisional orogenies. This paper addresses possible and hitherto unexplored cause-effect relationships between oroclinal bending of an originally linear orogenic belt and lithospheric thinning and delamination based on an example from the Western European Variscan Belt (WEVB). We suggest that late- to post-orogenic bending of the lithosphere around a vertical axis may cause thickening and eventual detachment of the lithospheric root of orogenic belts such as the WEVB. The proposed hypothesis is consistent with the chronology of tectonic, metamorphic, magmatic and hydrothermal events recorded in the WEVB.
spa
Orocimales y delaminación: relaciones y efectos
journal article
URL
https://docta.ucm.es/bitstreams/100227b4-ebc7-4647-a79a-947fdf344596/download
File
MD5
93ea1b4e0581493dd03c6b80dee3c04e
705838
application/pdf
Páginas desdeGeo_temas_6_3sge-4.pdf
URL
https://docta.ucm.es/bitstreams/4122079d-7169-47ba-a425-ed62abf36623/download
File
MD5
3f4241d1cc45af69d0e3fd12b4a53d40
21100
text/plain
Páginas desdeGeo_temas_6_3sge-4.pdf.txt