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Limestone-turbidites of the Variscan orogenic front: caused by a continent-continent-collision?

Author
EDER, W1 ; HINZ, K
[1] Inst. Geologie, 3400 Göttingen, Germany
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. 322

Scientific domain
Geology; Geophysics
Document type
Conference Paper
Language
English
Keyword (fr)
Calcaire Carbonifère inf Contrôle tectonique Courant turbidité Dévonien Flysch Milieu eau peu profonde Milieu marin Orogénie hercynienne Phase varisque Subsidence Turbidites Collision continent-continent Europe Primaire Roche carbonatée Roche clastique Roche sédimentaire
Keyword (en)
limestone Lower Carboniferous structural controls turbidity currents Devonian flysch shallow-water environment marine environment Hercynian Orogeny Variscan phase subsidence turbidite Europe Paleozoic carbonate rocks clastic rocks sedimentary rocks
Keyword (es)
Calcáreo Carbonifero inf Control tectónico Corriente turbiedad Devónico Flysch(geología) Medio agua poco profunda Medio marino Orogenia hercínica Fase varisca Subsidencia Turbidita Europa Primario Roca carbonatada Roca clástica Roca sedimentaria
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
4021554

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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