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Abstract

A new system for logging the geophysical properties of marine sediment cores allows both whole cores and split cores to be measured in a nondestructive fashion. The current sensor configuration measures compressional (P) wave velocity (500 kHz), bulk density (using gamma-ray attenuation), and magnetic susceptibility at user-defined sample intervals down the core. Split-core logging gives more reliable results than whole core logging as it mostly eliminates core-slumping effects that can lead to spurious results; it also gives higher resolution magnetic susceptibility readings.

Year of Publication
1998
Journal
Geo-Marine Letters
Volume
18
Number of Pages
70-77
ISBN Number
0276-0460
URL
http://dx.doi.org/10.1007/s003670050054
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