Correlacion Magnetoestratigráfica de las Sedimentitas Neogenas Aflorantes en la Cuenca do
Rodeo - Iglesia (San Juan - Argentina)

G.H. Ré; S.P. Barredo

doi:10.3997/2214-4609-pdb.324.734

Correlacion Magnetoestratigráfica de las Sedimentitas Neogenas Aflorantes en la Cuenca do Rodeo - Iglesia (San Juan - Argentina)
By G.H. Ré and S.P. Barredo
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 3rd International Congress of the Brazilian Geophysical Society, Nov 1993, cp-324-00140
DOI: https://doi.org/10.3997/2214-4609-pdb.324.734

Abstract

La Cuenca de Rodeo-Iglesia fue caracterizada como una piggiback basiin por Beer (1989) y Beer et al. (1990) que se encuentra geológica y geográficamente, limitada por la Cordillera Frontal (al Oeste) y por la Precordillera (al Este) (ver. Fig. 1). En este ambiente tectónico, la sedimentación terciaria se encuentra representada por el Grupo Iglesia, de edad mio-pliocena. Este Grupo está constituido por las Formaciones Las Flores y Lomas del Campanario (según Wetten, 1975: Contreras et al 1990).

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1993-11-07

2024-04-23

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Correlacion Magnetoestratigráfica de las Sedimentitas Neogenas Aflorantes en la Cuenca do Rodeo - Iglesia (San Juan - Argentina)

Abstract

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The natural combination of full and image‐based waveform inversion

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture