Kinematics of the Pyrenean pseudo-arc and Gibraltar arc through upper Paleozoic and Creataceous-Eocene Pyrenean sequences and the closure of Western Tethys
- Author
- BOURROUILH, R
Univ. Bordeaux I, CIBAMAR, France - Conference title
- 29th international geological congress (Kyoto, 24 August - 3 September 1992)
- Conference name
- International geological congress (29 ; Kyoto 1992-08-24)
- Source
29th international geological congress (Kyoto, 24 August - 3 September 1992). 1992 ; 2Vol ; p. 472
- Scientific domain
- Geology; Geophysics
- Document type
- Conference Paper
- Language
- English
- Keyword (fr)
- Arc volcanique Cinématique Compression tectonique Lithostratigraphie Marge continentale Mouvement plaque Paléogène Plaque Africaine Primaire sup Roche sédimentaire Tectonostratigraphie Téthys Europe Gibraltar Tertiaire
- Keyword (en)
- volcanic arcs kinematics compression tectonics lithostratigraphy continental margin plate movement Paleogene African Plate upper Paleozoic sedimentary rocks tectonostratigraphy Tethys Europe Gibraltar Tertiary
- Keyword (es)
- Cinemática Compresión tectónica Litoestratigrafía Margen continental Movimiento placa Paleógeno Placa Africana Primario sup Roca sedimentaria Tethys Europa Gibraltar Terciario
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01I Stratigraphy
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01L Tectonics. Structural geology. Plate tectonics
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 4022299
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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