New temporal constraints on the rotation of the Peruvian central Andes obtained from paleomagnetism

Orlando Efrain Macedo Sánchez; J. Surmont; C. Kissel; C. Laj

doi:10.1029/92GL01070

New temporal constraints on the rotation of the Peruvian central Andes obtained from paleomagnetism

Orlando Efrain Macedo Sánchez, J. Surmont, C. Kissel, C. Laj

Resultado de la investigación: Contribución a una revista › Artículo › revisión exhaustiva

18 Citas (Scopus)

Resumen

New paleomagnetic data from middle Eocene to middle Miocene volcanic and plutonic formations of the Western Cordillera of Central Peru document a counterclockwise rotation of 11°±7.4°. This rotation, similar to previous results reported for the northern Peruvian margin, is post middle‐Miocene in age. It is thus coeval with the acceleration of the Andean uplift and supports Isacks' model.

Idioma original	Inglés
Páginas (desde-hasta)	1875-1878
Número de páginas	4
Publicación	Geophysical Research Letters
Volumen	19
N.º	18
DOI	https://doi.org/10.1029/92GL01070
Estado	Publicada - 23 set. 1992
Publicado de forma externa	Sí

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abstract = "New paleomagnetic data from middle Eocene to middle Miocene volcanic and plutonic formations of the Western Cordillera of Central Peru document a counterclockwise rotation of 11°±7.4°. This rotation, similar to previous results reported for the northern Peruvian margin, is post middle‐Miocene in age. It is thus coeval with the acceleration of the Andean uplift and supports Isacks' model.",

author = "{Macedo S{\'a}nchez}, {Orlando Efrain} and J. Surmont and C. Kissel and C. Laj",

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T1 - New temporal constraints on the rotation of the Peruvian central Andes obtained from paleomagnetism

AU - Macedo Sánchez, Orlando Efrain

AU - Surmont, J.

AU - Kissel, C.

AU - Laj, C.

PY - 1992/9/23

Y1 - 1992/9/23

N2 - New paleomagnetic data from middle Eocene to middle Miocene volcanic and plutonic formations of the Western Cordillera of Central Peru document a counterclockwise rotation of 11°±7.4°. This rotation, similar to previous results reported for the northern Peruvian margin, is post middle‐Miocene in age. It is thus coeval with the acceleration of the Andean uplift and supports Isacks' model.

AB - New paleomagnetic data from middle Eocene to middle Miocene volcanic and plutonic formations of the Western Cordillera of Central Peru document a counterclockwise rotation of 11°±7.4°. This rotation, similar to previous results reported for the northern Peruvian margin, is post middle‐Miocene in age. It is thus coeval with the acceleration of the Andean uplift and supports Isacks' model.

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DO - 10.1029/92GL01070

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AN - SCOPUS:0027041227

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VL - 19

SP - 1875

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JO - Geophysical Research Letters

JF - Geophysical Research Letters

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ER -

New temporal constraints on the rotation of the Peruvian central Andes obtained from paleomagnetism

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