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- W2328857547 abstract "We made a gravimetric model, on a section which crossed through the Andean Cordillera, Pampean Ranges and Precordillera in an west to east direction, at -30° latitude south and 71° at 65° longitude west. The response of gravimetric model of the crust, fixed to the curve of the Bouguer anomaly upward continuation at 40km in height, which would correspond to the moho ondulations. This result was compared with the crustal thickness obtained by means of: (1) the Moho depths given by the apparent phase velocities Pn (Fromm et al., 2004)and (2) receiver function of wave S (Heit et al., 2008). In This study evaluated the gravimetric effect of the three cortical models compared with the regional Bouguer anomaly. The conclusions reveal that the major discrepancy between the models is produced in the Cuyania terrane, principally in the Precordillera zone. This includes the PACH and HEDI seismological stations and on minor measurement to the RINC station, located in the Famatina terrane. In accordance with the existing geological information, the Precordillera is a thinskin structure, whith a decollement horizon at 18km of depth." @default.
- W2328857547 created "2016-06-24" @default.
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- W2328857547 date "2009-01-01" @default.
- W2328857547 modified "2023-10-15" @default.
- W2328857547 title "Modelo Gravimétrico 2D Y Su Comparación Con Espesores Corticales Sísmicos En Una Sección A Los 30 ° De Latitud Sur" @default.
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- W2328857547 doi "https://doi.org/10.3997/2214-4609-pdb.195.1471_evt_6year_2009" @default.
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