Paleogeographic and tectonic evolution of the Iberian massif during Carboniferous time.

M. Julivert

Paleogeographic and tectonic evolution of the Iberian massif during Carboniferous time.

M. Julivert

Departament de Geologia

Producció científica: Contribució a revista › Article › Recerca › Avaluat per experts

2 Cites (Scopus)

Resum

The Iberian segment of the Hercynian foldbelt is formed by two branches with opposite polarity, and this seems to be generally true all along the belt. These zones were frontal zones of active deposition during the building of the Hercynian chain. The Carboniferous within the Hercynian foldbelt shows the following succesion of facies: 1) condensed, 2) turbiditic (culm=flysch), 3) paralic, and 4) fluviatile and limnic facies. The change from one facies to another is not synchronous in the different zones of the belt.-from Author

Idioma original	Anglès
Pàgines (de-a)	49-68
Revista	9ieme congres international de stratigraphie et de geologie du Carbonifere, Washington/Champaign-Urbana, 1979: compte rendu. Vol. 1
Estat de la publicació	Publicada - 1 de gen. 1984

Com citar-ho

@article{25936f8ad0cc4e638831d975c504479d,

title = "Paleogeographic and tectonic evolution of the Iberian massif during Carboniferous time.",

abstract = "The Iberian segment of the Hercynian foldbelt is formed by two branches with opposite polarity, and this seems to be generally true all along the belt. These zones were frontal zones of active deposition during the building of the Hercynian chain. The Carboniferous within the Hercynian foldbelt shows the following succesion of facies: 1) condensed, 2) turbiditic (culm=flysch), 3) paralic, and 4) fluviatile and limnic facies. The change from one facies to another is not synchronous in the different zones of the belt.-from Author",

author = "M. Julivert",

year = "1984",

month = jan,

day = "1",

language = "English",

pages = "49--68",

}

TY - JOUR

T1 - Paleogeographic and tectonic evolution of the Iberian massif during Carboniferous time.

AU - Julivert, M.

PY - 1984/1/1

Y1 - 1984/1/1

N2 - The Iberian segment of the Hercynian foldbelt is formed by two branches with opposite polarity, and this seems to be generally true all along the belt. These zones were frontal zones of active deposition during the building of the Hercynian chain. The Carboniferous within the Hercynian foldbelt shows the following succesion of facies: 1) condensed, 2) turbiditic (culm=flysch), 3) paralic, and 4) fluviatile and limnic facies. The change from one facies to another is not synchronous in the different zones of the belt.-from Author

AB - The Iberian segment of the Hercynian foldbelt is formed by two branches with opposite polarity, and this seems to be generally true all along the belt. These zones were frontal zones of active deposition during the building of the Hercynian chain. The Carboniferous within the Hercynian foldbelt shows the following succesion of facies: 1) condensed, 2) turbiditic (culm=flysch), 3) paralic, and 4) fluviatile and limnic facies. The change from one facies to another is not synchronous in the different zones of the belt.-from Author

M3 - Article

SP - 49

EP - 68

JO - 9ieme congres international de stratigraphie et de geologie du Carbonifere, Washington/Champaign-Urbana, 1979: compte rendu. Vol. 1

JF - 9ieme congres international de stratigraphie et de geologie du Carbonifere, Washington/Champaign-Urbana, 1979: compte rendu. Vol. 1

ER -

Paleogeographic and tectonic evolution of the Iberian massif during Carboniferous time.

Resum

Fingerprint

Com citar-ho