A Joint Inversion Method of Electromagnetic,ÿGeodetic and Seismological Data for the Study of Planetary Interiors

Mathematics – Logic

Scientific paper

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1227 Planetary Geodesy And Gravity (5420, 5714, 6019), 3260 Inverse Theory, 5109 Magnetic And Electrical Properties, 6225 Mars, 7207 Core And Mantle

Scientific paper

A new method is developed to determine the structure of telluric planetary interiors. It is based on the joint inversion of data from in situÿgeophysical experiments and laboratory measurements. We infer conditional probability densities of the parameters governingÿthe internal structure by stochastic inversion. This multi-parameters approach is quite generic and canÿbe applied to any telluric planet. We illustrate it here withÿsimulated data of the future Netlanderÿmission to Mars. The simulated data come from the electromagnetic, geodetic and seismological experiments. This approach is free of any a priori assumption regarding theÿtemperature profile of the planetary mantle. From the inferred conditional probabilities we estimate the mineralogy and the temperature profile for the mantle as well as the sulfur weight fraction and the temperature profile for a possible liquid core.

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