A magnetic time line for Mars

Computer Science

Scientific paper

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Scientific paper

In this paper, we re-examine the magnetic signature of impact craters as it was measured by MGS. We carefully selected the measurements in order to isolate the spatial variations. We then compare the magnetic field observed directly above these volcanoes or basins to the one measured around them. We conclude that the martian dynamo was most likely active when they were formed, between 3.7 and 3.8 Gyrs ago.

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