Crater is a geologic structure in solid bodies (including the terrestrial planets, moons, and
asteroids) formed by hyper-speed impact, and the impact process is extremely important to …

The Moon is a unique body in our Solar System that allows us to groundtruth remotesensing
data (eg, crater size–frequency distributions, or CSFDs, crater/rock degradation rates …

By using high-resolution altimetric measurements of the Moon, we produced a catalog of all
impact craters≥ 20 kilometers in diameter on the lunar surface and analyzed their …

Vesta is a large differentiated rocky body in the main asteroid belt that accreted within the
first few million years after the formation of the earliest solar system solids. The Dawn …

The identification of impact craters on planetary surfaces provides important information
about their geological history. Most studies have relied on individual analysts who map and …

Impact basin formation is a fundamental process in the evolution of the Moon and records
the history of impactors in the early solar system. In order to assess the stratigraphy …

The geological record of early Mars displays a variety of features that indicate fundamental
differences from more recent conditions. These include evidence for:(1) widespread …

Abstract NASA's Double Asteroid Redirection Test (DART) spacecraft is planned to impact
the natural satellite of (65803) Didymos, Dimorphos, at around 23: 14 UTC on 2022 …

The global population of lunar craters> 20 km in diameter was analyzed by Head et
al.,(2010) to correlate crater distribution with resurfacing events and multiple impactor …

Analyzing the density of impact craters on planetary surfaces is the only known technique for
learning their ages remotely. As a result, crater statistics have been widely analyzed on the …