Zobrazeno 1 - 10
of 92
pro vyhledávání: '"D. Frizon de Lamotte"'
Publikováno v:
Tectonics
Tectonics, American Geophysical Union (AGU), 2019, 38 (8), pp.2668-2702. ⟨10.1029/2018TC005472⟩
Tectonics (0278-7407) (American Geophysical Union (AGU)), 2019-08, Vol. 38, N. 8, P. 2668-2702
Tectonics, American Geophysical Union (AGU), 2019, 38 (8), pp.2668-2702. ⟨10.1029/2018TC005472⟩
Tectonics (0278-7407) (American Geophysical Union (AGU)), 2019-08, Vol. 38, N. 8, P. 2668-2702
International audience; We revisit the nature, structure, and evolution of the Ionian Basin and its surrounding passive margins (Apulia, Eastern Sicily/Malta, and Cyrenaica margins). Relying on geological observations (wells, dredges, and dives) and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7c8bae4a1bac704e5e1ea7606c30ff2e
https://hal.archives-ouvertes.fr/hal-02324095/document
https://hal.archives-ouvertes.fr/hal-02324095/document
Autor:
Jean Besse, F. Leparmentier, M. Lescanne, Marianne Greff-Lefftz, D. Frizon de Lamotte, Frédéric Gueydan, S. Vicente De Gouveia
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2018, 487, pp.210-220. ⟨10.1016/j.epsl.2018.01.030⟩
Earth and Planetary Science Letters, Elsevier, 2018, 487, pp.210-220. ⟨10.1016/j.epsl.2018.01.030⟩
International audience; Rifts are often associated with ancient traces of hotspots, which are supposed to participate to the weakening of the lithosphere. We investigated the expected past trajectories followed by three hotspots (Afar, East-Africa an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de1c5940df11965440fe36e78fa331d1
https://hal.archives-ouvertes.fr/hal-01801626
https://hal.archives-ouvertes.fr/hal-01801626
Publikováno v:
Journal of Petroleum Geology. 36:309-334
The High Zagros in Iran, the most internal zone of the Zagros fold-and-thrust belt, is discontinuous and is only present in two mountainous areas located in the central and eastern parts of the belt respectively. Compared to other zones of the Zagros
Publikováno v:
Tectonophysics. :63-77
We present a study integrating petrophysical measurements along a general N–S section of the Corbieres–Minervois fold and thrust belt (NE Pyrenees, France) in order to study the petrofabric of weakly deformed sediments. We focus on the relationsh
Autor:
Omar Saddiqi, F. Negro, D. Frizon de Lamotte, Samira Sebti, Daniel F. Stockli, Finlay M. Stuart, J.-P. Schaer, Jocelyn Barbarand, J.P.T. Foeken, Geoffrey Ruiz
Publikováno v:
Terra Nova. 23:35-41
Terra Nova, 23, 35–41, 2011 Abstract To put constraints on the Mesozoic to recent growth of the Anti-Atlas system, we investigated the temperature–time history of rocks by applying extensive low-temperature thermochronological analysis to three P
Akademický článek
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Autor:
Charles Aubourg, Rudy Swennen, D. Frizon de Lamotte, B. Saint-Bezar, Philippe Robion, Ronan Hébert
Publikováno v:
Journal of Structural Geology. 24:1507-1520
An investigation of the anisotropy of magnetic susceptibility (AMS) of hematite-bearing sandstones has been carried out along two fault-propagation folds located at the front of the High Atlas Belt (Goulmima area, Morocco). It reveals two types of un
Publikováno v:
Geological Magazine
Geological Magazine, Cambridge University Press (CUP), 2014, 151 ((5):), pp.885-898 (IF 2,270)
Geological Magazine, Cambridge University Press (CUP), 2014, 151 ((5):), pp.885-898 (IF 2,270)
The absence of a sedimentary record on large cratonic areas often prevents the reconstruction of the history of their vertical movements. The Reguibat Rise, belonging to the West African Craton, is typically a large basement high, whose Meso-Cenozoic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b08bd2492e32dedd2222b2c6e4e75d70
https://hal.science/hal-01064916
https://hal.science/hal-01064916
Publikováno v:
Geological Society, London, Special Publications. 156:1-14
Publikováno v:
Journal of Structural Geology. 20:999-1011
The kinematics of several tip line folds situated along the South Atlas Front near Goulmima (Morocco) is established using both forward modelling and analysis of syn-folding deformation. From the Sahara foreland to the Atlas, the two successive major