  High temperature impact melt breccias from the Rochechouart (France)
meteorite crater record magnetization component with antipodal, normal and
reverse polarities. The corresponding paleomagnetic pole for this component
lies between the 220 Ma and 210 Ma reference poles on the Eurasian apparent
polar wander path, consistent with the 214 $\pm$ 8 Ma 40Ar/39Ar age of the
crater. Late Triassic tectonic reconstructions of the Eurasian and North
American plates place this pole within 95% confidence limits of the
paleomagnetic pole from the Manicouagan (Canada) meteorite impact crater, which
is dated at 214 $\pm$ 1 Ma. Together, these observations reinforce the
hypothesis of a Late Triassic, multiple meteorite impact event on Earth.
