We investigate lunar internal structure models which are consistent with the seismic and the selenodetic data and thermodynamic constraints. The seismic travel time data constrain crustal and mantle structures and composition, while selenodetic data are expected to contribute to infer the structure below the deep moonquake region.
CITATION STYLE
Kronrod, E., Matsumoto, K., Kuskov, O., Kronrod, V., Yamada, R., & Kamata, S. (2018). Joint inversion of geophysical (seismic and selenodetic) and geochemical data for internal structure and composition of the Moon. In IOP Conference Series: Materials Science and Engineering (Vol. 468). Institute of Physics Publishing. https://doi.org/10.1088/1757-899X/468/1/012015
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