Volcanism is the most important endogenic geological process of the Moon, which is closely
related to its internal structure and thermal history. Lunar volcanism is one of the most …

The lunar nearside has been investigated by many uncrewed and crewed missions, but the
farside of the Moon remains poorly known. Lunar farside exploration is challenging because …

This work presents the results of the Lunar Regolith Penetrating Radar (LRPR), installed at
the bottom of the Chang'E-5 (CE-5) lander, which is the first antenna-array radar deployed …

Mars' surface is characterized by a weathered layer of regolith and exposed rock exposures
that are the results of long‐term geological processes. The Mars Rover Penetrating Radar …

The Lunar Gravitational-wave Antenna (LGWA) is a proposed array of next-generation
inertial sensors to monitor the response of the Moon to gravitational waves (GWs). Given the …

We revealed the layered structure of the upper three hundred meters of the lunar surface in
the South Pole‐Aitken Basin by using the measurements from the Lunar Penetrating Radar …

Ground-penetrating radar (GPR) is becoming a mainstream tool in planetary exploration,
and one of the few in-situ planetary geophysical methods. There are currently three missions …

Yutu-2–the rover from the Chang'E-4 mission–is the longest operational Lunar rover, and
the first rover to land on the far side of the Moon. It is the second planetary rover to be …

The Moon-based ground-penetrating radar (GPR) onboard the Chang'E-4 (CE-4) Yutu-2
rover has deployed on the Moon's far side, providing an unprecedented opportunity to study …

The Yutu-2 rover, part of the Chang'e-4 (CE-4) mission to the lunar farside, has been
exploring the Von Kármán crater (VK) within the South Pole-Aitken (SPA) gathering data on …