Earth’s mantle occupies most of its volume, connecting the deep, inaccessible core to the surface. Its convection regulates the planet’s temperature, magnetic field, chemical distribution, and habitability conditions. Changes in convective regimes therefore have profound implications for Earth’s evolution and our interpretation of the geologic record. In this talk, I ...
The crustal magnetic anomalies near the lunar crater Gerasimovich are among the highest-magnitude anomalies on the Moon. Previous work has suggested they formed from the deposition and magnetization of ejecta from the Crisium basin, which is antipodal to the region. In this talk, I will describe the correlation between topographic ...
