Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Oligocene - Pliocene"'
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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This paper presents a detailed provenance analysis of the 6.5-km thick Oligocene–Pliocene foreland succession in the north Dezful embayment in Zagros, Iran. Using petrography, geochemistry, and paleoflow analysis, we determined three provenance shi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c13fc8131785416af72703a38a906ec8
Autor:
Andrić, Nevena, Sant, K., Mațenco, L., Mandic, O., Tomljenović, B., Pavelić, D., Hrvatović, H., Demir, V., Ooms, J., Tectonics, Paleomagnetism
Publikováno v:
Marine and Petroleum Geology, 83, 305. Elsevier BV
The coupled tectonic and depositional history of extensional basins is usually described in terms of stratigraphic sequences linked with the activity of normal faults. This depositional-kinematic interplay is less understood in basins bounded by majo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d05a77dd8113ed67a5910bde1e051f08
https://www.bib.irb.hr/868328
https://www.bib.irb.hr/868328
Autor:
Norberto Malumian, Eduardo B. Olivero
Publikováno v:
Revista geológica de Chile, Volume: 32, Issue: 1, Pages: 117-129, Published: JAN 2005
Revista geológica de Chile v.32 n.1 2005
SciELO Chile
CONICYT Chile
instacron:CONICYT
Revista geológica de Chile v.32 n.1 2005
SciELO Chile
CONICYT Chile
instacron:CONICYT
En el área del río Irigoyen, dentro de la faja plegada de los Andes Fueguinos, afloran sedimentitas oligocenas, plegadas y de ambiente marino profundo, y sedimentitas del Mioceno Superior-Plioceno, de contrastante estructura subhorizontal y ambient
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5a9332f325779f508a99b7d298fcdfd
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082005000100007&lng=en&tlng=en
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082005000100007&lng=en&tlng=en
Conference
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Autor:
Benmakhlouf, M., Chalouan, Ahmed
Tetouan-MartHpost-nappes basin is opened by two rifting stages: the first in late Oligocene-Burdigalian times, is accompanied by ductile normal faults in Aquitanian-Burdigalian rocks; the second of post Burdigaiian and pre-PHocene age, has produced t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::9dbe50fe02d966218447185d63eaab0f
Autor:
Benmakhlouf, M., Chalouan, Ahmed
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
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Tetouan-MartHpost-nappes basin is opened by two rifting stages: the first in late Oligocene-Burdigalian times, is accompanied by ductile normal faults in Aquitanian-Burdigalian rocks; the second of post Burdigaiian and pre-PHocene age, has produced t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::9dbe50fe02d966218447185d63eaab0f
http://hdl.handle.net/10272/13876
http://hdl.handle.net/10272/13876
Akademický článek
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