The GHMT includes the nuclear magnetic remanence sonde (NMRS), which measures total
magnetic field, and the susceptibility measurement sonde (SUMS), which measures the
magnetic susceptibility from induction.
The Leg 194 logging plan has been designed to achieve the following objectives:
Core-log-seismic correlation. A detailed correlation between cores, logs, and the extensive
suite of high-quality seismic reflection data (including the closely spaced site survey grids and
regional two-dimensional lines) will be critical for understanding the three-dimensional
architecture of the Marion Plateau sequences and for compiling a detailed sequence stratigraphy.
Accordingly, check-shot (WST) surveys, at 30 to 50 m spacing, should be run at all sites.
Detailed description of cored sequences. Integrated interpretation of the FMS and
geophysical logs (triple-combo) will provide an essential complement to drill cores for
describing the lithostratigraphy, particularly in intervals where core recovery is incomplete.
Geophysical logs will also be important for characterizing the lithostratigraphic response of the
carbonate sediments to sea-level and climatic fluctuations.
Characterization of sedimentary diagenesis. Sedimentary diagenesis in carbonates is
expressed through changes in porosity and chemical precipitation of soluble elements (such as
uranium) that lead to large changes in log properties seen on sonic, resistivity, density, and
neutron gamma-ray logs.
Detection of terrigenous sediment input to the sedimentary section. The Marion Plateau is
a mixed carbonate-siliciclastic depositional environment; thus, the GHMT tool will be useful for
detecting variations in terrigenous sediment content intermixed with the platform and pelagic
carbonate sediments, particularly in those intervals characterized by low core recovery. These
data will be also be useful for intersite sediment correlation.
Assessment of fracture networks and basic fluid properties. Fine-scale characteristics of
sedimentary bedding, including pore spaces, bioturbation, and fractures, will be imaged using
the FMS. The assessment of fracture networks and fluids will be accomplished using sonic and
resistivity logs that, together with FMS images, should help achieve leg fluid-flow objectives.