Natural Science

Natural Science

ISSN Print: 2150-4091
ISSN Online: 2150-4105
www.scirp.org/journal/ns
E-mail: ns@scirp.org
"Stripe of normal mechanisms for crustal earthquakes with M ≤ 3.5 flanking the western side of the thrust front zone in the Andes backarc"
written by Silvina Nacif, Enrique Triep, Renzo Furlani, Silvana Spagnotto,
published by Natural Science, Vol.5 No.8A, 2013
has been cited by the following article(s):
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[1] Long‐Term Lithospheric Strength and Upper‐Plate Seismicity in the Southern Central Andes, 29°–39° S
Geochemistry …, 2022
[2] Within plate seismicity analysis in the segment between the high Cordillera and the Precordillera of northern Mendoza (Southern Central Andes)
Geodesy and Geodynamics, 2018
[3] Geodesy and Geodynamics
2017
[4] Three-dimensional approach to understanding the relationship between the Plio–Quaternary stress field and tectonic inversion in the Triassic Cuyo Basin, Argentina
2015
[5] Three-dimensional approach to understanding the relationship between the Plio-Quaternary stress field and tectonic inversion in the Triassic Cuyo Basin …
2015
[6] El frente orogénico activo de Los Andes centrales a la latitud de la ciudad de Mendoza (32° 50'-33° S)
2014
[7] EL FRENTE OROGéNICO ACTIVO DE LOS ANDES CENTRALES A LA LATITUD DE LA CIUDAD DE MENDOZA (32o50′-33o S)
MENDOZA, DE, Stella M. Moreiras, Laura B. Giambiagi, Silvana Spagnotto, Silvina Nacif, José Mescua, and Rafael Toural Dapoza, 2014
[8] Current active front of the Central Andes at Mendoza city latitude (32o50?-33oS).
Andean Geology, 2014
[9] El frente orogénico activo de Ios Andes centrales a la latitud de la ciudad de Mendoza (32° 50'-33° S)
Andean Geology, 2014
[10] Current active front of the Central Andes at Mendoza city latitude (32º50ʼ-33ºS).
2014
[11] El frente orogénico activo de los Andes centrales a la latitud de la ciudad de Mendoza (32º50ʼ-33ºS)
Andean Geology, 2014
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