Zobrazeno 1 - 2
of 2
pro vyhledávání: '"syn-collisional lithospheric delamination"'
Autor:
Guillot François, Averbuch Olivier, Dubois Michel, Durand Cyril, Lanari Pierre, Gauthier Arnaud
Publikováno v:
BSGF - Earth Sciences Bulletin, Vol 191, p 26 (2020)
To provide a better picture of the active geodynamics along the Variscan suture zones during the late collisional stage (particularly regarding the evolution of the orogenic system towards HT conditions), we focused here on vaugnerites, which consist
Externí odkaz:
https://doaj.org/article/9764c72773514600b4f594c117b74ce5
Autor:
Guillot, François, Averbuch, Olivier, Dubois, Michel, Durand, Cyril, Lanari, Pierre, Gauthier, Arnaud, Averbuch, O., Lardeaux, J.M.
Publikováno v:
BSGF-Earth Sciences Bulletin, Vol 191, p 26 (2020)
Guillot, François; Averbuch, Olivier; Dubois, Michel; Durand, Cyril; Lanari, Pierre; Gauthier, Arnaud; Averbuch, O.; Lardeaux, J.M. (2020). Zircon age of vaugnerite intrusives from the Central and Southern Vosges crystalline massif (E France): contribution to the geodynamics of the European Variscan belt. BSGF-Earth Sciences Bulletin, 191, p. 26. 10.1051/bsgf/2020027
Bulletin de la Société Géologique de France
Bulletin de la Société Géologique de France, Société géologique de France, 2020, 191, pp.26. ⟨10.1051/bsgf/2020027⟩
Bulletin de la Société Géologique de France, 2020, 191, pp.26. ⟨10.1051/bsgf/2020027⟩
Guillot, François; Averbuch, Olivier; Dubois, Michel; Durand, Cyril; Lanari, Pierre; Gauthier, Arnaud; Averbuch, O.; Lardeaux, J.M. (2020). Zircon age of vaugnerite intrusives from the Central and Southern Vosges crystalline massif (E France): contribution to the geodynamics of the European Variscan belt. BSGF-Earth Sciences Bulletin, 191, p. 26. 10.1051/bsgf/2020027
Bulletin de la Société Géologique de France
Bulletin de la Société Géologique de France, Société géologique de France, 2020, 191, pp.26. ⟨10.1051/bsgf/2020027⟩
Bulletin de la Société Géologique de France, 2020, 191, pp.26. ⟨10.1051/bsgf/2020027⟩
International audience; To provide a better picture of the active geodynamics along the Variscan suture zones during the late collisional stage (particularly regarding the evolution of the orogenic system towards HT conditions), we focused here on va