Aegean tectonics: Strain localisation, slab tearing and trench retreat

Autor: Jolivet, Laurent, Faccenna, Claudio, Huet, Benjamin, Labrousse, Loïc, Le Pourhiet, Laetitia, Lacombe, Olivier, Lecomte, Emmanuel, Burov, Evguenii, Denèle, Yoann, Brun, Jean-Pierre, Philippon, Mélody, Paul, Anne, Salaün, Gwenaëlle, Karabulut, Hayrullah, Piromallo, Claudia, Monié, Patrick, Gueydan, Frédéric, Okay, Aral I., Oberhänsli, Roland, Pourteau, Amaury, Augier, Romain, Gadenne, Leslie, Driussi, Olivier

Publikováno v: In Tectonophysics 19 June 2013 597-598:1-33

Polysilazane derived micro/nano Si 3N 4/SiC composites

Autor: Zemanová, Matilda, Lecomte, Emmanuel, Šajgalı́k, Pavol, Riedel, Ralf

Publikováno v: In Journal of the European Ceramic Society 2002 22(16):2963-2968

Détachements et failles normales a faible pendage : cinématique et localisation de la déformation, approche de terrain et modélisation numérique. Exemple des Cyclades

Autor: Lecomte, Emmanuel

Publikováno v: Tectonique. Université Pierre et Marie Curie-Paris VI, 2010. Français
Tectonique. Université Pierre et Marie Curie-Paris VI, 2010. Français. ⟨NNT : ⟩

Several low-angle normal faults (dipping less than 30°) have been described in extensional continental domain since their discovery in the Basin and Range Province (USA). Although field observations suggest that normal faults can be reactivated with

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::57190371b4c70f6abdc16bf3eb28b2d6
https://tel.archives-ouvertes.fr/tel-00567978/file/PhDLecomte2010.pdf

A continuum mechanics approach to quantify brittle strain on weak faults: application to the extensional reactivation of shallow dipping discontinuities

Autor: Lecomte, Emmanuel, Le Pourhiet, Laetitia, Lacombe, Olivier, Jolivet, Laurent

Publikováno v: Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2011, 184, pp.1-11. ⟨10.1111/j.1365-246X.2010.04821.x⟩
Geophysical Journal International, 2011, 184, pp.1-11. ⟨10.1111/j.1365-246X.2010.04821.x⟩

International audience; A number of field observations suggest that sliding on fault planes may occur at very shallow dip in the brittle field. The existence of active low angle normal faults is much debated because (1) the classical theory of fault

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f2508f047ab3d68181576a65e1911764
https://hal-insu.archives-ouvertes.fr/insu-00564131/document

Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.