Retrieving "Paleomagnetic Paleosols" from the archives

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1. Magnetic Field Orientation

   Linked via "paleomagnetic paleosols"

   The path traced by the paleomagnetic pole relative to a specific continental mass over time is known as the Apparent Polar Wander (APW) curve-curve/). The shape of this curve defines the former latitude and longitude of the continent. When integrating the APW curves-curve/) of multiple terranes, discrepancies often arise, necessitating the introduction of tectonic adjustments to fit a coherent supercontinent model.
   For instance, modeling the accretio…