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author Brink, Jason
Jarrard, Richard D
author_facet Brink, Jason
Jarrard, Richard D
collection Datos científicos de ciencias marinas y ambientales
contents This paper reports measurements of velocity vs pressure and of bulk density, porosity, matrix density, and magnetic susceptibility in 18 core plugs from CRP-1. Comparison of our bulk densities with continuous whole-core density records shows very good agreement. Core-plug measurements of matrix density permit conversion of the whole-core density record to porosity. Agreement between our magnetic susceptibility measurements and the continuous, whole-core data is excellent. In contrast, our atmospheric pressure measurements of P-wave velocity are ~10% faster than whole-core data obtained at the same pressure. Our measurements of velocity versus pressure indicate that in situ P-wave velocities are probably only 1-3% higher than those measured at atmospheric pressure. Although the Miocene section has undergone significant exhumation, we do not observe typical exhumation signatures of anomalously low initial velocities followed by microcrack closing as pressure is increased. Instead, velocity response to pressure appears to be dominated by a small amount of post-exhumation cementation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_54728
institution PANGAEA
language en
publishDate 1998
publisher PANGAEA
record_format pangaea
spellingShingle Petrophysical measurements on core plug samples of sediment core CRP-1 (Table 1)
Brink, Jason
Jarrard, Richard D
16 km ENE Cape Roberts; Calculated; Calculated from mass/volume; Cape Roberts Project; Core wireline system; CRP; CRP-1; CRP-1__Campaign; CWS; Density, grain; Density, wet bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Magnetic susceptibility, volume; off Cape Roberts, Ross Sea, Antarctica; Porosity; Sampling/drilling ice; Susceptibility unit Kappabridge KLY-2; Velocity, compressional/shear wave ratio; Velocity, compressional wave; Velocity, shear wave
This paper reports measurements of velocity vs pressure and of bulk density, porosity, matrix density, and magnetic susceptibility in 18 core plugs from CRP-1. Comparison of our bulk densities with continuous whole-core density records shows very good agreement. Core-plug measurements of matrix density permit conversion of the whole-core density record to porosity. Agreement between our magnetic susceptibility measurements and the continuous, whole-core data is excellent. In contrast, our atmospheric pressure measurements of P-wave velocity are ~10% faster than whole-core data obtained at the same pressure. Our measurements of velocity versus pressure indicate that in situ P-wave velocities are probably only 1-3% higher than those measured at atmospheric pressure. Although the Miocene section has undergone significant exhumation, we do not observe typical exhumation signatures of anomalously low initial velocities followed by microcrack closing as pressure is increased. Instead, velocity response to pressure appears to be dominated by a small amount of post-exhumation cementation.
title Petrophysical measurements on core plug samples of sediment core CRP-1 (Table 1)
topic 16 km ENE Cape Roberts; Calculated; Calculated from mass/volume; Cape Roberts Project; Core wireline system; CRP; CRP-1; CRP-1__Campaign; CWS; Density, grain; Density, wet bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Magnetic susceptibility, volume; off Cape Roberts, Ross Sea, Antarctica; Porosity; Sampling/drilling ice; Susceptibility unit Kappabridge KLY-2; Velocity, compressional/shear wave ratio; Velocity, compressional wave; Velocity, shear wave
url https://doi.org/10.1594/PANGAEA.54728