Gravity crustal model for an andean section at 32° s considering upper mantle lateral density variation



Título del documento: Gravity crustal model for an andean section at 32° s considering upper mantle lateral density variation
Revista: Revista brasileira de geofisica
Base de datos: PERIÓDICA
Número de sistema: 000279634
ISSN: 0102-261X
Autores: 1
Instituciones: 1Universidad Nacional de San Juan, Facultad de Ciencias Exactas, San Juan, Bahía Blanca. Argentina
Año:
Periodo: May-Ago
Volumen: 18
Número: 2
Paginación: 107-116
País: Brasil
Idioma: Inglés
Tipo de documento: Artículo
Enfoque: Experimental, analítico
Resumen en inglés Up to date, three gravity models for the Andean section at 32° south latitude have been published. Two of them did not have seismic reflection/refraction data to constrain the subsurface geometry. The other one included seismic data to fit thicknesses and determined density contrasts using velocity-density curves. Furthermore, all previous models assumed a homogeneous mantle. In this paper a new gravity model is computed for a two-layer crust of the Andean section at the 32° south latitude. It involves new seismic depths for the Andean foreland, recent worldwide velocity-density relationships and a simple model of the subducting slab. The shape of the Nazca plate is defined from available contour maps of the Wadati-Benioff zone of western South America. The slab density contrast with respect to the surrounding mantle is estimated to be +1.6% (3.5-5.5% velocity anomaly), which reproduces the long-wavelength gravity anomaly. The modelled crustal structure is analyzed taking into account interpretations derived from seismic data. Crustal thicknesses vary from about 50 km in the Sierras Pampeanas to 71 km in the Andean belt. According to this model, most of the thickening takes place in the upper crustal layer, in the region between the Precordillera and Pampean Ranges. These results agree with recent seismological data. A Cenozoic lower crust shortening of 146 km to an initial crust 40 km thick is calculated from the computed crustal roots. This estimate of shortening is within 10% of previous calculations from gravity models. Also, i
Disciplinas: Geociencias
Palabras clave: Geofísica,
Sismología y vulcanología,
Campo de gravedad,
Andes,
Modelos gravimétricos,
Manto superior,
Placa de Nazca
Keyword: Earth sciences,
Geophysics,
Seismology and volcanology,
Gravity field,
Andes,
Upper mantle,
Nazca plate
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