Martian meteorite launch: High-speed ejecta from small craters

被引:147
作者
Head, JN
Melosh, HJ
Ivanov, BA
机构
[1] Univ Arizona, Dept Planetary Sci, Tucson, AZ 85721 USA
[2] Raytheon Missile Syst, Tucson, AZ 85734 USA
[3] Russian Acad Sci, Inst Dynam Geospheres, Moscow 117939, Russia
关键词
D O I
10.1126/science.1077483
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
We performed high-resolution computer simulations of impacts into homogeneous and layered martian terrain analogs to try to account for the ages and characteristics of the martian meteorite collection found on Earth. We found that craters as small as similar to3 kilometers can eject similar to10(7) decimeter-sized fragments from Mars, which is enough to expect those fragments to appear in the terrestrial collection. This minimum crater diameter is at least four times smaller than previous estimates and depends on the physical composition of the target material. Terrain covered by a weak layer such as an impact-generated regolith requires larger, therefore rarer, impacts to eject meteorites. Because older terrain is more likely to be mantled with such material, we estimate that the martian meteorites will be biased toward younger ages, which is consistent with the meteorite collection.
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收藏
页码:1752 / 1756
页数:5
相关论文
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