Magnetotelluric inversion constrained by seismic data in the Tucumán Basin (Andean Foothills, 27°S, NW Argentina)

A magnetotelluric (MT) profile and conventional seismic reflection lines are used to characterize the sedimentary basin across the Andean foothills in the Tucumán Plain. This basin is a depocenter surrounded by crystalline basement and filled with a several‐kilometer‐thick sedimentary sequence. Beca...

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Veröffentlicht in:Journal of Geophysical Research: Solid Earth 2007-09, Vol.112 (B9), p.n/a
Hauptverfasser: Favetto, Alicia, Pomposiello, Cristina, Booker, John, Rossello, Eduardo A.
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Sprache:eng
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