Zobrazeno 1 - 3
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pro vyhledávání: '"Ana Caro Montero"'
Publikováno v:
Geodesy and Geodynamics, Vol 9, Iss 1, Pp 77-92 (2018)
The Sierras de Córdoba are the easternmost uplifted ranges of the Sierras Pampeanas geological province of Argentina. They are composed of a Neoproterozoic–Paleozoic basement arranged in north–south aligned mountain ranges, limited by west-verge
Externí odkaz:
https://doaj.org/article/fe0344b869134e72a77ce50a6ec7a878
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Geodesy and Geodynamics, Vol 9, Iss 1, Pp 77-92 (2018)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Geodesy and Geodynamics, Vol 9, Iss 1, Pp 77-92 (2018)
The Sierras de Córdoba are the easternmost uplifted ranges of the Sierras Pampeanas geological province of Argentina. They are composed of a Neoproterozoic–Paleozoic basement arranged in north–south aligned mountain ranges, limited by west-verge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ca84bbf73238a242b0e5945dd75029e
https://www.sciencedirect.com/science/article/pii/S1674984717301003
https://www.sciencedirect.com/science/article/pii/S1674984717301003
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland deformation, over 700 km from the Chile trench. This deformation started at c. 340 Ma through basement faults, thrusts and reactivation of normal faults o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a71c386786865670966629bd133b067d
https://www.cambridge.org/core/journals/geological-magazine/article/reactivation-inversion-and-basement-faulting-and-thrusting-in-the-sierras-pampeanas-of-cordoba-argentina-during-andean-flat-slab-deformation/0612DC5C78EED51EDB76A2DA67391496
https://www.cambridge.org/core/journals/geological-magazine/article/reactivation-inversion-and-basement-faulting-and-thrusting-in-the-sierras-pampeanas-of-cordoba-argentina-during-andean-flat-slab-deformation/0612DC5C78EED51EDB76A2DA67391496