In July 2011 the Dawn spacecraft entered orbit around the Main Belt asteroid 4 Vesta utilizing three different instruments to map the asteroid [1]. The Main Belt is the source region of most impactors in the inner solar system [2]. We compare the obtained crater size-frequency distribution (CSFD) of Vesta with that of the Moon and other Main Belt asteroids such as 951 Gaspra, 243 Ida, and 21 Lutetia. We also compare our results of crater counting on Vesta with K/Ar-Ar reset ages of HED meteorites, which most likely originated from Vesta [3]. To properly compare the lunar CSFD with that of the asteroids we applied scaling laws [4] to account for various impact velocities, surface gravities as well as material properties between the investiga...
The Dawn mission has completed its Survey and High-Altitude Mapping Orbit (HAMO) phases at Vesta, re...
Dawn space mission will provide the first, detailed data of two of the major bodies in the Main Belt...
In this paper, we present a global database of craters larger than 0.7 km in diameter on the surface...
In July 2011 the Dawn spacecraft entered orbit around the Main Belt asteroid 4 Vesta. Dawn has been ...
The Dawn mission showed asteroid 4 Vesta to be an extensively cratered body, ancient in age, with cr...
We derived model functions for the crater production size-frequency distribution and chronology of t...
The Dawn spacecraft now in orbit has revealed the asteroid 4 Vesta to be a heavily cratered object, ...
entered orbit around the Main Belt asteroid 4 Vesta. Dawn has been designed to map the asteroid Vest...
Vesta is a large differentiated rocky body in the main asteroid belt that accreted within the first ...
Context. The forthcoming arrival of the NASA’s Dawn spacecraft to Ceres and Vesta means that these u...
Context. The forthcoming arrival of the NASA's Dawn spacecraft to Ceres and Vesta means that these u...
The Dawn spacecraft arrived at Vesta on July 16, 2011 to study the asteroid with a Framing Camera (F...
The Ninth Symposium on Polar Science/Ordinary sessions: [OA] Antarctic meteorites / Hayabusa, Wed. 5...
We used Dawn spacecraft data to identify and delineate geological units and landforms in the Marcia ...
abstract: We used Dawn spacecraft data to identify and delineate geological units and landforms in t...
The Dawn mission has completed its Survey and High-Altitude Mapping Orbit (HAMO) phases at Vesta, re...
Dawn space mission will provide the first, detailed data of two of the major bodies in the Main Belt...
In this paper, we present a global database of craters larger than 0.7 km in diameter on the surface...
In July 2011 the Dawn spacecraft entered orbit around the Main Belt asteroid 4 Vesta. Dawn has been ...
The Dawn mission showed asteroid 4 Vesta to be an extensively cratered body, ancient in age, with cr...
We derived model functions for the crater production size-frequency distribution and chronology of t...
The Dawn spacecraft now in orbit has revealed the asteroid 4 Vesta to be a heavily cratered object, ...
entered orbit around the Main Belt asteroid 4 Vesta. Dawn has been designed to map the asteroid Vest...
Vesta is a large differentiated rocky body in the main asteroid belt that accreted within the first ...
Context. The forthcoming arrival of the NASA’s Dawn spacecraft to Ceres and Vesta means that these u...
Context. The forthcoming arrival of the NASA's Dawn spacecraft to Ceres and Vesta means that these u...
The Dawn spacecraft arrived at Vesta on July 16, 2011 to study the asteroid with a Framing Camera (F...
The Ninth Symposium on Polar Science/Ordinary sessions: [OA] Antarctic meteorites / Hayabusa, Wed. 5...
We used Dawn spacecraft data to identify and delineate geological units and landforms in the Marcia ...
abstract: We used Dawn spacecraft data to identify and delineate geological units and landforms in t...
The Dawn mission has completed its Survey and High-Altitude Mapping Orbit (HAMO) phases at Vesta, re...
Dawn space mission will provide the first, detailed data of two of the major bodies in the Main Belt...
In this paper, we present a global database of craters larger than 0.7 km in diameter on the surface...