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- W2336684311 abstract "Tunas Formation (Permian) outcrops at the east area of Sierras Australes (Buenos Aires province, Argentina) and it continues on subsurface in the Claromeco Basin. It is integrated by fine to medium sandstones alternating with mudrocks, which contains detritic hematite. A preliminary AMS study is carried out to evaluate the internal deformation, at different stratigraphic levels of Tunas Formation, with the aim of determining direction and magnitude of the main efforts which had acted on this formation. Preliminary results show that the Kmax poles trend NW-SE, close to the regional axial fold trend and Kmin have good consistence with the pole of the bedding plane, placed in a girdle perpendicular to Kmax. The Kmin positions changes from the horizontal at the bottom of the sequence to the vertical at the top of the sequence showing a clear sedimentary fabric. These changes in the Kmin axis positions have proved a decrease of the deformation intensity toward the foreland basin. The NW trend of the Kmax axes implies a SW-NE compression in concordance with the regional compression pattern along the Gondwanaland margin." @default.
- W2336684311 created "2016-06-24" @default.
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- W2336684311 date "2011-01-01" @default.
- W2336684311 modified "2023-09-26" @default.
- W2336684311 title "ANÁLISIS DE ANISOTROPÍA DE SUSCEPTIBILIDAD MAGNÉTICA (ASM) Y COMPACTACIÓN EN LA FORMACIÓN TUNAS, SIERRAS AUSTRALES DE LA PROVINCIA DE BUENOS AIRES, ARGENTINA" @default.
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