Subsurface Density Structure of the Orientale Basin Revealed by 3D Gravity Inversion of GRAIL Data
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Results for the Orientale Basin region of the Moon. This dataset comprises subsurface density structures from the GRAIL Bouguer anomaly using 3D gravity inversion. The density structures were computed using spherical harmonic expansions, degrees and orders 2–660 and 60–660, enabling assessment of both long- and short-wavelength components of the gravity field.
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Zenodo创建时间：
2026-03-25
