Asymmetric Craters on the Dwarf Planet Ceres-Results of Second Extended Mission Data Analysis

被引:2
作者
Krohn, Katrin [1 ]
Jaumann, Ralf [1 ,2 ]
Wickhusen, Kai [1 ]
Otto, Katharina A. [1 ]
Kersten, Elke [1 ]
Stephan, Katrin [1 ]
Wagner, Roland J. [1 ]
Raymond, Carol A. [3 ]
Russell, Christopher T. [4 ]
机构
[1] Deutsch Zentrum Luft & Raumfahrt, Inst Planetary Res, D-12489 Berlin, Germany
[2] Free Univ Berlin, Inst Geol Sci Planetary Sci & Remote Sensing, D-12249 Berlin, Germany
[3] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[4] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
基金
美国国家航空航天局;
关键词
crater formation on small bodies; cratering processes; influence of slopes; asteroids; dwarf planets; asymmetrical cratering; XM2; IMPACT; EVOLUTION; VESTA; SHAPE;
D O I
10.3390/geosciences9110475
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
After almost three years of successful operation on Ceres, the Dawn spacecraft entered its last orbits around the dwarf planet and obtained a set of high-resolution images of 3 to 5 m/pixel. These images reveal a variety of morphologic features, including a set of asymmetric crater morphologies as observed earlier in the mission on the asteroid Vesta. We identified 269 craters, which are located between 60 degrees N to 60 degrees S latitude and 197 degrees E to 265 degrees E longitude, and investigated their morphological characteristics using a digital terrain model (DTM). These craters range in diameter from 0.30 to 4.2 km, and exhibit a sharp crater rim on the uphill side and a smooth one on the downhill side. We found that all asymmetric craters are formed on a sloping surface with the majority appearing at slope angles between 5 and 20 degrees. This implies that, as observed on Vesta, the topography is the main cause for these asymmetries.
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页数:11
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