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pro vyhledávání: '"Jean Aubouin"'
Autor:
Jean Aubouin
Publikováno v:
Tectonophysics. 183:1-7
Between the Asian and Australian continents on the western side and the general subduction of the Central Pacific on the eastern side, the west Pacific presents two types of subduction: towards the continents and towards the ocean. As a consequence,
Autor:
Jean Aubouin
Publikováno v:
Earth-Science Reviews. 36:254-255
Autor:
Jean Aubouin
Publikováno v:
Bulletin de la Société Géologique de France. :501-515
Autor:
Jean Aubouin
Publikováno v:
Tectonophysics. 160:1-21
The main structures of a subduction zone are as follows. 1. (1) On the outer wall: faults, formed either by reactivation of the structural grain of the oceanic plate, when the latter is slightly oblique to the trench, or by a new fault network parall
Publikováno v:
Tectonophysics. 86:113-132
Short Sea-Beam survey cruises were conducted by the R.V. “Jean Charcot” in march 1980 along the Middle America Trench between Panama and Acapulco, with particular emphasis on the IPOD Legs 66 and 67 areas. These detailed mappings have revealed th
Publikováno v:
Bulletin de la Société Géologique de France. :179-190
Autor:
Richard W. Faas, Donald M. Hussong, Grant Blackinton, William E. Harrison, Joseph A. Curiale, Tsunemasa Shiki, Darrel S. Cowan, Jean Aubouin, Reinhard Hesse, Nikita Muzylov, Jacques Azema, Jean Westberg, William T. Coulbourn, Roland von Huene, Carlos A. Dengo, Peter R. Thompson, Jerry A. Carter, John W. Ladd
Publikováno v:
Geological Society, London, Special Publications. 10:121-129
Autor:
Jean Aubouin
Publikováno v:
Bulletin de la Société Géologique de France. :333-343
Autor:
Jean Aubouin, Drummond Matthews, Jean Mascle, Dimitri Mitropoulos, S. Monti, Nicolas Lyberis, Vincent Renard, Henri Got, Xavier Le Pichon, Yossi Mart, Ken Hsu, Georges Chronis, Pandelis Tsoflias, Jacques Angelier
Publikováno v:
Earth and Planetary Science Letters. 44:441-450
Preliminary results of a multi-narrow beam survey of the Hellenic trench system, in the Eastern Mediterranean, are presented. The southwestern Ionian branch is divided in small basins, partly filled with Pleistocene sediments. The morphology suggests
Publikováno v:
Earth and Planetary Science Letters. 67:211-218
The results of DSDP Legs 67 and 84, during which a transect of holes was drilled across the Middle America Trench off Guatemala, show no accretion at the front of that subduction zone since early Eocene time. The tectonic evolution of the trench incl