Abstract
GOCE satellite data and EGM2008 model are used to calculate the gravity anomaly and the vertical gravity gradient, both corrected by the topographic effect, in order to delineate main tectonic features related to density variations. In particular, using the Bouguer anomaly from GOCE, we calculated the crust–mantle discontinuity obtaining elastic thicknesses in the frame of the isostatic lithospheric flexure model applying the convolution method approach. Results show substantial variations in the density, compositional and thermal structure, and isostatic and flexural behavior of the continental lithosphere along the Southern Andes and adjacent foreland region.
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Acknowledgements
Authors acknowledge the use of the GMT mapping software of Wessel and Smith (1998) and to Dr. L. Uieda, Dr. J. Janak, Dr. M. Sprlak, and Dr. Prof. C. Braitenberg for their usefull softwares. The authors would like to thank to CONICET and the Ministerio de Ciencia y Técnica–Agencia de Promoción Científica y Tecnológica, PICT07-1903 for financial support.
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Álvarez, O., Lince Klinger, F., Gimenez, M., Ruiz, F., Martinez, P. (2016). Density and Thermal Structure of the Southern Andes and Adjacent Foreland from 32° to 55°S Using Earth Gravity Field Models. In: Folguera, A., Naipauer, M., Sagripanti, L., C. Ghiglione, M., Orts, D., Giambiagi, L. (eds) Growth of the Southern Andes. Springer Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-23060-3_2
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