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Crustal structure and tectonic setting of the south central Andes from gravimetric analysis
Authors:Cecilia Weidmann  Silvana Spagnotto  Orlando Álvarez  Marcos Sánchez  Federico Lince Klinger  Mario Giménez  Patricia Martínez
Institution:Consejo Nacional de Investigaciones, Científcas y Técnicas, Argentina;CONICET, Instituto Geofísico Sismológico Volponi, Universidad Nacional de San Juan, Argentina
Abstract:Based on terrestrial gravity data, in this paper we prepared a map of Bouguer anomalies, which was filtered to separate shallow and deep gravity sources. Based on a density model and gravimetric inversion techniques, the discontinuous crust-mantle boundary and the top of crystalline basement were modeled. Subsequently, the equivalent elastic thickness (Te) was evaluated, considering information from the crust-mantle discontinuity and topographic load, finding high Te values in the eastern Andean foothills and west of the Velasco range. These results are consistent with the positive isostatic and residual Bouguer anomaly values, which suggest the presence of high-density rocks in the mid-to upper crust. In addition, petrographic and geochemical analysis conducted in surface outcrops suggest a mantle origin.
Keywords:gravedad  isostasia  espesor elástico equivalente  Andes centrales  modelo cortical  Sierras Pampeanas  gravity  isostasy  equivalent elastic thickness  southern Andes  crustal model  Sierras Pampeanas
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