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Identification of possible source craters for Martian meteorite ALH84001

机译:识别Martian Meteorite alh84001的可能源陨石坑

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Twelve meteorites are currently believed to be samples from the Martian surface. Eleven of these meteorites, called the shergottites, nakhlites, and chassignites (or SNC meteorites), have young formation ages (≤1.3 X 10~9 yr). The twelfth Martian meteorite, ALH84001, is very ancient (4.5 X 10~9 yr). The differences in formation ages and composition suggest that these twelve meteorites came from at least two and possibly three or more different source craters on Mars. The eleven SNC meteorites are from a young volcanic area, likely the Tharsis Region in the western hemisphere of Mars. Previous studies have identified up to nine possible source craters for these meteorites. The old Martian meteorite, ALH84001, must be from the ancient terrain of Mars, which covers about 40% of the plane primarily in the southern hemisphere. A search through the 42,283-entry Catalog of Large Martian Impact Craters has produced 23 possible source craters, which upon further photogeologic analysis has been reduced to two strong candidates and six runners-up.
机译:目前认为十二个陨石是来自火星表面的样品。这些陨石11个称为Shergottites,Nakhlites和豆类(或SNC陨石),具有年轻的形成年龄(≤1.3x 10〜9。第十二火星陨石,秋季84001,非常古老(4.5 x 10〜9,Yr)。形成年龄和组合物的差异表明,这些十二颗陨石来自火星上的至少两个,可能是三个或更多不同的源陨石坑。 11个SNC陨石来自一座年轻的火山区域,可能是马斯西半球的Tharsis地区。以前的研究已经确定了这些陨石的九种可能的源陨石坑。老火星陨石,亚山,必须来自火星的古代地形,主要占地面积约40%的飞机,主要是在南半球。通过大型火星冲击陨石坑的42,283进入目录的搜索产生了23种可能的源陨石坑,这在进一步的光学学分析后已经减少到两个强大的候选人和六个赛跑者。

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