(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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Bibliographic Details
Main Authors: Jarrard, Richard D, Paulsen, Timothy S, Wilson, Terry
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.465903
https://doi.org/10.1594/PANGAEA.465903
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.465903
record_format openpolar
spelling 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
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