A PREDICTION OF MARS SEISMICITY FROM SURFACE FAULTING
A PREDICTION OF MARS SEISMICITY FROM SURFACE FAULTING
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DOI：
10.1126/science.258.5084.979
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发表时间：
1992-11-06
期刊：
影响因子：
56.9
通讯作者：
TRALLI, DM
中科院分区：
文献类型：
--
作者：
GOLOMBEK, MP;BANERDT, WB;TRALLI, DM
火星的浅层地震活动是通过测量整个地质时期火星表面可见断层的总滑动来估计的。地震活动是根据月球表面结构和测量的月球地震活动（包括整个地震岩石圈）进行估计的。结果表明，火星是地震活跃的今天，有足够数量的可检测marsquakes允许地震调查其内部。
The shallow seismicity of Mars has been estimated by measurement of the total slip on faults visible on the surface of the planet throughout geologic time. Seismicity was calibrated with estimates based on surface structures on the moon and measured lunar seismicity that includes the entire seismogenic lithosphere. Results indicate that Mars is seismically active today, with a sufficient number of detectable marsquakes to allow seismic investigations of its interior.