Physical properties of sediment core CRP-2A ...

In this paper the relationship between whole-core compressional wave velocities and gamma-ray attenuation porosities of sediments cored at CRP-2/2A is examined, and compared with results from CRP-1, CRP-2/2A core-plug samples, and global models for velocity/porosity relationships of marine sediments...

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Bibliographic Details
Main Author: Niessen, Frank
Format: Dataset
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.55713
https://doi.pangaea.de/10.1594/PANGAEA.55713
id ftdatacite:10.1594/pangaea.55713
record_format openpolar
spelling ftdatacite:10.1594/pangaea.55713 2024-09-15T17:44:51+00:00 Physical properties of sediment core CRP-2A ... Niessen, Frank 1999 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.55713 https://doi.pangaea.de/10.1594/PANGAEA.55713 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Porosity Density, wet bulk Velocity, compressional wave Susceptibility Core wireline system Multi-Sensor Core Logger 17, GEOTEK CRP-2 Sampling/drilling from ice Cape Roberts Project CRP dataset Supplementary Dataset Dataset 1999 ftdatacite https://doi.org/10.1594/pangaea.55713 2024-08-01T11:03:26Z In this paper the relationship between whole-core compressional wave velocities and gamma-ray attenuation porosities of sediments cored at CRP-2/2A is examined, and compared with results from CRP-1, CRP-2/2A core-plug samples, and global models for velocity/porosity relationships of marine sediments. The high degree of data scatter observed in the velocity/porosity relationship of CRP-1 core is even larger in CRP-2/2A core. The general pattern of the velocity/porosity relationship is similar in CRP-2/2A whole core and core plug measurements. Despite scatter, all data indicate a strong primary dependence of velocity on porosity. This relationship appears to be independent of lithology except for sections with zero porosity and porosity >0.6, which are attributed to large lonestones and lapillistones, respectively. Core velocity/porosity patterns of CRP-1 and CRP-2/2A are very similar for sediments from the same age interval (19-23 Ma), both characterized by relatively low velocities (mostly between 2 and 3 ... : Supplement to: Niessen, Frank; Kopsch, Conrad; Polozek, Kerstin (2000): Velocity and porosity from CRP-2/2A core logs, Victoria Land Basin, Antarctica. Terra Antartica, 7(3), 241-253 ... Dataset Antarc* Antarctica antartic* Victoria Land DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Porosity
Density, wet bulk
Velocity, compressional wave
Susceptibility
Core wireline system
Multi-Sensor Core Logger 17, GEOTEK
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
spellingShingle DEPTH, sediment/rock
Porosity
Density, wet bulk
Velocity, compressional wave
Susceptibility
Core wireline system
Multi-Sensor Core Logger 17, GEOTEK
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
Niessen, Frank
Physical properties of sediment core CRP-2A ...
topic_facet DEPTH, sediment/rock
Porosity
Density, wet bulk
Velocity, compressional wave
Susceptibility
Core wireline system
Multi-Sensor Core Logger 17, GEOTEK
CRP-2
Sampling/drilling from ice
Cape Roberts Project CRP
description In this paper the relationship between whole-core compressional wave velocities and gamma-ray attenuation porosities of sediments cored at CRP-2/2A is examined, and compared with results from CRP-1, CRP-2/2A core-plug samples, and global models for velocity/porosity relationships of marine sediments. The high degree of data scatter observed in the velocity/porosity relationship of CRP-1 core is even larger in CRP-2/2A core. The general pattern of the velocity/porosity relationship is similar in CRP-2/2A whole core and core plug measurements. Despite scatter, all data indicate a strong primary dependence of velocity on porosity. This relationship appears to be independent of lithology except for sections with zero porosity and porosity >0.6, which are attributed to large lonestones and lapillistones, respectively. Core velocity/porosity patterns of CRP-1 and CRP-2/2A are very similar for sediments from the same age interval (19-23 Ma), both characterized by relatively low velocities (mostly between 2 and 3 ... : Supplement to: Niessen, Frank; Kopsch, Conrad; Polozek, Kerstin (2000): Velocity and porosity from CRP-2/2A core logs, Victoria Land Basin, Antarctica. Terra Antartica, 7(3), 241-253 ...
format Dataset
author Niessen, Frank
author_facet Niessen, Frank
author_sort Niessen, Frank
title Physical properties of sediment core CRP-2A ...
title_short Physical properties of sediment core CRP-2A ...
title_full Physical properties of sediment core CRP-2A ...
title_fullStr Physical properties of sediment core CRP-2A ...
title_full_unstemmed Physical properties of sediment core CRP-2A ...
title_sort physical properties of sediment core crp-2a ...
publisher PANGAEA
publishDate 1999
url https://dx.doi.org/10.1594/pangaea.55713
https://doi.pangaea.de/10.1594/PANGAEA.55713
genre Antarc*
Antarctica
antartic*
Victoria Land
genre_facet Antarc*
Antarctica
antartic*
Victoria Land
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.55713
_version_ 1810492521955983360