Magneto Statistics

Magnetostratigraphy is a geophysical connection method used to date sedimentary and volcanic successions. The technique works by gathering focused examples at estimated interims all through the area. The examples are broke down to decide their trademark remanent polarization (ChRM), that is, the extremity of Earth's attractive field at the time a stratum was stored. This is conceivable in light of the fact that volcanic streams obtain a thermoremanent charge and silt get a depositional remanent polarization, both of which mirror the bearing of the Earth's field at the season of arrangement. This strategy is ordinarily used to date arrangements that for the most part need fossils or interbedded molten shake