Core derived downhole logs for holes CRP-2 and CRP-2A
In the northern McMurdo Sound (Ross Sea, Antarctica), the CRP-2/2A drillhole targeted the western margin of the Victoria Land Basin to investigate Neogene to Palaeogene climatic and tectonic history by obtaining continuous core and downhole logs. Well logging of CRP-2/2A has provided a complete and...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.57235 2023-05-15T14:04:42+02:00 Core derived downhole logs for holes CRP-2 and CRP-2A Bücker, Christian J LATITUDE: -77.005982 * LONGITUDE: 163.719450 * DATE/TIME START: 1998-10-01T00:00:00 * DATE/TIME END: 1998-11-25T14:20:00 * MINIMUM DEPTH, sediment/rock: 11.00 m * MAXIMUM DEPTH, sediment/rock: 624.60 m 2000-08-25 text/tab-separated-values, 48984 data points https://doi.pangaea.de/10.1594/PANGAEA.57235 https://doi.org/10.1594/PANGAEA.57235 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.57235 https://doi.org/10.1594/PANGAEA.57235 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Bücker, Christian J; Jarrard, Richard D; Wonik, Thomas; Brink, Jason (2000): Analysis of downhole logging data from CRP-2/2A, Victoria Land Basin, Antarctica: a multivariate statistical approach. Terra Antartica, 7(3), 299-310, hdl:10013/epic.28289.d001 14.2 km at 096° true from Cape Roberts Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS Density wet bulk DEPTH sediment/rock Downhole logging Event label Magnetic susceptibility volume Natural gamma ray Neutron Porosity off Cape Roberts Ross Sea Antarctica Potassium Resistivity deep Sampling/drilling from ice Thorium Uranium Velocity compressional wave Dataset 2000 ftpangaea https://doi.org/10.1594/PANGAEA.57235 2023-01-20T07:36:09Z In the northern McMurdo Sound (Ross Sea, Antarctica), the CRP-2/2A drillhole targeted the western margin of the Victoria Land Basin to investigate Neogene to Palaeogene climatic and tectonic history by obtaining continuous core and downhole logs. Well logging of CRP-2/2A has provided a complete and comprehensive dataset of in situ geophysical measurements. This paper describes the evaluation and interpretation of the downhole logging data using multivariate statistical methods. Two major types of multivariate statistical methods were each yielding a different perspective: (1) Factor analysis was used as an objective tool for classification of the drilled sequence based on physical and chemical properties. The factor logs are mirroring the basic geological controls (i.e., grain size, porosity, clay mineralogy) behind the measured geophysical properties, thereby making them easier to interpret geologically. (2) Cluster analysis of the logs groups similar downhole geophysical properties into one cluster, delineating individual logging or sedimentological units. These objectively and independently defined units, or statistical electrofacies, are helpful in differentiating lithological and sedimentological characterisations (e.g. grain size, provenance). The multivariate statistical methods of factor and cluster analysis proved to be powerful tools for fast, reliable, and objective characterisation of downhole geophysical properties at CRP-2/2A, resulting in interpretations which are consistent with sedimentological findings. Dataset Antarc* Antarctica McMurdo Sound Ross Sea Victoria Land PANGAEA - Data Publisher for Earth & Environmental Science Ross Sea Victoria Land McMurdo Sound Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) Roberts Cape ENVELOPE(163.200,163.200,-77.033,-77.033) ENVELOPE(163.719450,163.719450,-77.005982,-77.005982) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
14.2 km at 096° true from Cape Roberts Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS Density wet bulk DEPTH sediment/rock Downhole logging Event label Magnetic susceptibility volume Natural gamma ray Neutron Porosity off Cape Roberts Ross Sea Antarctica Potassium Resistivity deep Sampling/drilling from ice Thorium Uranium Velocity compressional wave |
spellingShingle |
14.2 km at 096° true from Cape Roberts Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS Density wet bulk DEPTH sediment/rock Downhole logging Event label Magnetic susceptibility volume Natural gamma ray Neutron Porosity off Cape Roberts Ross Sea Antarctica Potassium Resistivity deep Sampling/drilling from ice Thorium Uranium Velocity compressional wave Bücker, Christian J Core derived downhole logs for holes CRP-2 and CRP-2A |
topic_facet |
14.2 km at 096° true from Cape Roberts Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS Density wet bulk DEPTH sediment/rock Downhole logging Event label Magnetic susceptibility volume Natural gamma ray Neutron Porosity off Cape Roberts Ross Sea Antarctica Potassium Resistivity deep Sampling/drilling from ice Thorium Uranium Velocity compressional wave |
description |
In the northern McMurdo Sound (Ross Sea, Antarctica), the CRP-2/2A drillhole targeted the western margin of the Victoria Land Basin to investigate Neogene to Palaeogene climatic and tectonic history by obtaining continuous core and downhole logs. Well logging of CRP-2/2A has provided a complete and comprehensive dataset of in situ geophysical measurements. This paper describes the evaluation and interpretation of the downhole logging data using multivariate statistical methods. Two major types of multivariate statistical methods were each yielding a different perspective: (1) Factor analysis was used as an objective tool for classification of the drilled sequence based on physical and chemical properties. The factor logs are mirroring the basic geological controls (i.e., grain size, porosity, clay mineralogy) behind the measured geophysical properties, thereby making them easier to interpret geologically. (2) Cluster analysis of the logs groups similar downhole geophysical properties into one cluster, delineating individual logging or sedimentological units. These objectively and independently defined units, or statistical electrofacies, are helpful in differentiating lithological and sedimentological characterisations (e.g. grain size, provenance). The multivariate statistical methods of factor and cluster analysis proved to be powerful tools for fast, reliable, and objective characterisation of downhole geophysical properties at CRP-2/2A, resulting in interpretations which are consistent with sedimentological findings. |
format |
Dataset |
author |
Bücker, Christian J |
author_facet |
Bücker, Christian J |
author_sort |
Bücker, Christian J |
title |
Core derived downhole logs for holes CRP-2 and CRP-2A |
title_short |
Core derived downhole logs for holes CRP-2 and CRP-2A |
title_full |
Core derived downhole logs for holes CRP-2 and CRP-2A |
title_fullStr |
Core derived downhole logs for holes CRP-2 and CRP-2A |
title_full_unstemmed |
Core derived downhole logs for holes CRP-2 and CRP-2A |
title_sort |
core derived downhole logs for holes crp-2 and crp-2a |
publisher |
PANGAEA |
publishDate |
2000 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.57235 https://doi.org/10.1594/PANGAEA.57235 |
op_coverage |
LATITUDE: -77.005982 * LONGITUDE: 163.719450 * DATE/TIME START: 1998-10-01T00:00:00 * DATE/TIME END: 1998-11-25T14:20:00 * MINIMUM DEPTH, sediment/rock: 11.00 m * MAXIMUM DEPTH, sediment/rock: 624.60 m |
long_lat |
ENVELOPE(-70.467,-70.467,-68.950,-68.950) ENVELOPE(163.200,163.200,-77.033,-77.033) ENVELOPE(163.719450,163.719450,-77.005982,-77.005982) |
geographic |
Ross Sea Victoria Land McMurdo Sound Cape Roberts Roberts Cape |
geographic_facet |
Ross Sea Victoria Land McMurdo Sound Cape Roberts Roberts Cape |
genre |
Antarc* Antarctica McMurdo Sound Ross Sea Victoria Land |
genre_facet |
Antarc* Antarctica McMurdo Sound Ross Sea Victoria Land |
op_source |
Supplement to: Bücker, Christian J; Jarrard, Richard D; Wonik, Thomas; Brink, Jason (2000): Analysis of downhole logging data from CRP-2/2A, Victoria Land Basin, Antarctica: a multivariate statistical approach. Terra Antartica, 7(3), 299-310, hdl:10013/epic.28289.d001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.57235 https://doi.org/10.1594/PANGAEA.57235 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.57235 |
_version_ |
1766275949175767040 |