(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North
CRP-3 cores were not orientated with respect to North during coring operations. However, borehole televiewer (BHTV) logging did obtain azimuthally orientated images of the borehole wall, and core processing included digital imaging of the outer surface of 85% of the cores. Images of many individual...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.465903 2024-09-15T18:32:31+00:00 (Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North Jarrard, Richard D Paulsen, Timothy S Wilson, Terry LATITUDE: -77.006000 * LONGITUDE: 163.719000 * DATE/TIME START: 1999-10-09T00:00:00 * DATE/TIME END: 1999-11-19T00:00:00 * MINIMUM DEPTH, sediment/rock: 219.470 m * MAXIMUM DEPTH, sediment/rock: 899.365 m 2001 text/tab-separated-values, 132 data points https://doi.pangaea.de/10.1594/PANGAEA.465903 https://doi.org/10.1594/PANGAEA.465903 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.465903 https://doi.org/10.1594/PANGAEA.465903 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Jarrard, Richard D; Paulsen, Timothy S; Wilson, Terry (2001): Orientation of CRP-3 core, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 161-166, hdl:10013/epic.28211.d001 Angle Cape Roberts Project Confidence Core wireline system CRP CRP-3 CWS Depth bottom/max sediment/rock top/min Number of observations Ross Sea Sampling/drilling from ice Standard deviation dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.465903 2024-07-24T02:31:27Z CRP-3 cores were not orientated with respect to North during coring operations. However, borehole televiewer (BHTV) logging did obtain azimuthally orientated images of the borehole wall, and core processing included digital imaging of the outer surface of 85% of the cores. Images of many individual core segments can be digitally joined, or stitched, by rotating them to match the shapes of their adjoining surfaces and then closing the gap. By aligning features (fractures, bedding, and clasts) on stitched-core images with correlative features on orientated BHTV images, we reorientated 231 m of core, or 25% of the cored interval. We estimate that the orientation uncertainty is ±10° for entire stitched-core intervals, and ±15° for individual features such as a single fracture or palaeomagnetic sample. Reliability of core orientations was confirmed by comparing azimuths of bedding and fractures measured directly within these reorientated cores to those measured within orientated borehole televiewer images. Dataset Ross Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(163.719000,163.719000,-77.006000,-77.006000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Angle Cape Roberts Project Confidence Core wireline system CRP CRP-3 CWS Depth bottom/max sediment/rock top/min Number of observations Ross Sea Sampling/drilling from ice Standard deviation |
spellingShingle |
Angle Cape Roberts Project Confidence Core wireline system CRP CRP-3 CWS Depth bottom/max sediment/rock top/min Number of observations Ross Sea Sampling/drilling from ice Standard deviation Jarrard, Richard D Paulsen, Timothy S Wilson, Terry (Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
topic_facet |
Angle Cape Roberts Project Confidence Core wireline system CRP CRP-3 CWS Depth bottom/max sediment/rock top/min Number of observations Ross Sea Sampling/drilling from ice Standard deviation |
description |
CRP-3 cores were not orientated with respect to North during coring operations. However, borehole televiewer (BHTV) logging did obtain azimuthally orientated images of the borehole wall, and core processing included digital imaging of the outer surface of 85% of the cores. Images of many individual core segments can be digitally joined, or stitched, by rotating them to match the shapes of their adjoining surfaces and then closing the gap. By aligning features (fractures, bedding, and clasts) on stitched-core images with correlative features on orientated BHTV images, we reorientated 231 m of core, or 25% of the cored interval. We estimate that the orientation uncertainty is ±10° for entire stitched-core intervals, and ±15° for individual features such as a single fracture or palaeomagnetic sample. Reliability of core orientations was confirmed by comparing azimuths of bedding and fractures measured directly within these reorientated cores to those measured within orientated borehole televiewer images. |
format |
Dataset |
author |
Jarrard, Richard D Paulsen, Timothy S Wilson, Terry |
author_facet |
Jarrard, Richard D Paulsen, Timothy S Wilson, Terry |
author_sort |
Jarrard, Richard D |
title |
(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
title_short |
(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
title_full |
(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
title_fullStr |
(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
title_full_unstemmed |
(Table 1) Core intervals of sediment core CRP-3 that have been stitched and reorientated to North |
title_sort |
(table 1) core intervals of sediment core crp-3 that have been stitched and reorientated to north |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.465903 https://doi.org/10.1594/PANGAEA.465903 |
op_coverage |
LATITUDE: -77.006000 * LONGITUDE: 163.719000 * DATE/TIME START: 1999-10-09T00:00:00 * DATE/TIME END: 1999-11-19T00:00:00 * MINIMUM DEPTH, sediment/rock: 219.470 m * MAXIMUM DEPTH, sediment/rock: 899.365 m |
long_lat |
ENVELOPE(163.719000,163.719000,-77.006000,-77.006000) |
genre |
Ross Sea |
genre_facet |
Ross Sea |
op_source |
Supplement to: Jarrard, Richard D; Paulsen, Timothy S; Wilson, Terry (2001): Orientation of CRP-3 core, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 161-166, hdl:10013/epic.28211.d001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.465903 https://doi.org/10.1594/PANGAEA.465903 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.465903 |
_version_ |
1810474261100363776 |