Lunar Far Side

Under the Surface fine-grained Regolith, superpositions among these Crater Materials and mare Basalt Units establish shallow Regolith Stratigraphic sequences. The low-frequency data (CH-1, 60 MHz) show a deep Stratigraphic Structure to the depth of approx. 360 mt that indicates the previous Geological evolution history of the Von Kármán Crater.
The LPR results (will) provide an important scientific basis for understanding the Geological History of the Far Side of the Moon.