Figure F89. Downhole variation in magnetic susceptibility () and natural remanent magnetization (NRM) for the sedimentary units. Note that the diamagnetic contribution of calcite (-13.8 × 10-6 SI) has been subtracted from the susceptibility.
)
and natural remanent magnetization (NRM) for the sedimentary units. Note that
the diamagnetic contribution of calcite (-13.8 × 10-6 SI) has been
subtracted from the susceptibility.