Abstract
In the framework of several international research projects performed in Ross Sea (Antarctica) in the last years marine gravity data, high resolution reflection seismic lines and deep seismic sounding profiles have been acquired.
The gravity data set has been used to compute maps of Bouguer anomaly, isostatic anomaly, isostatic correction and local geoid undulations. Forward modelling of seismic and gravity data has been also used to compute the depths of the Crust-Mantle discontinuity.
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© 1997 Springer-Verlag Berlin Heidelberg
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Marson, I., Štoka, M., Velicogna, I., Coren, F., Zanolla, C. (1997). Gravity, Geoid, Isostasy and Moho Depth in the Ross Sea, Antarctica. In: Segawa, J., Fujimoto, H., Okubo, S. (eds) Gravity, Geoid and Marine Geodesy. International Association of Geodesy Symposia, vol 117. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-03482-8_48
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DOI: https://doi.org/10.1007/978-3-662-03482-8_48
Publisher Name: Springer, Berlin, Heidelberg
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