Background

Ocean Drilling Program Hole 910D was drilled on the crest of the southern Yermak Plateau at 80°15.881'N, 6°65.424'E, in 567.7 m water depth. This hole consists of three cores recovered with the advanced hydraulic piston corer (APC) and 15 cores recovered with the extended core barrel (XCB)...

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Bibliographic Details
Main Authors: Frank R. Rack, Rustan Finndin, Kate Moran
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.5488
http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.508.5488 2023-05-15T18:45:46+02:00 Background Frank R. Rack Rustan Finndin Kate Moran The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.5488 http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.5488 http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf text ftciteseerx 2021-02-07T01:19:00Z Ocean Drilling Program Hole 910D was drilled on the crest of the southern Yermak Plateau at 80°15.881'N, 6°65.424'E, in 567.7 m water depth. This hole consists of three cores recovered with the advanced hydraulic piston corer (APC) and 15 cores recovered with the extended core barrel (XCB), penetrating to a total depth of 160.6 meters below sea floor (mbsf). Three ear-lier holes were drilled at this site, but two of them (Holes 910A and 910B) failed to penetrate through a stiff horizon at about 20-24 mbsf, and a third hole (Hole 9IOC), drilled using the rotary core barrel (RCB), yielded poor core recovery in the upper 200 mbsf. As a first step in the study of individual core sections from Hole 910D, non-destructive, whole-core X-ray examinations were performed at the Atlantic Geoscience Center of the Bedford Institute of Oceanography in Dartmouth, Nova Scotia, Can-ada. Using a high-resolution video monitor, X-ray images of almost 96 m of core were visually examined and described; these X-ray images were simultaneously recorded on video tape for further digital processing and interpretation. Videotaped X-ray images of the Hole 910D core sections have been used to identify the relative position and size of indi-vidual clasts (>2 mm in diameter) and coarse sand layers, and to identify extensively bioturbated intervals, represented by bur-row traces in these cores. Solid particles>2 mm in diameter, were counted for successive 10-cm intervals of core using the video X-ray images. The X-ray images provide "ground truth " for making comparisons with other nondestructive measure-ments made on these cores using sensors mounted on the multisensor track (MST), and for identifying changes in depositional environments at this site. Text Yermak plateau Unknown Bedford ENVELOPE(-67.150,-67.150,-66.467,-66.467) Lier ENVELOPE(19.343,19.343,69.775,69.775) Yermak Plateau ENVELOPE(5.000,5.000,81.250,81.250)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Ocean Drilling Program Hole 910D was drilled on the crest of the southern Yermak Plateau at 80°15.881'N, 6°65.424'E, in 567.7 m water depth. This hole consists of three cores recovered with the advanced hydraulic piston corer (APC) and 15 cores recovered with the extended core barrel (XCB), penetrating to a total depth of 160.6 meters below sea floor (mbsf). Three ear-lier holes were drilled at this site, but two of them (Holes 910A and 910B) failed to penetrate through a stiff horizon at about 20-24 mbsf, and a third hole (Hole 9IOC), drilled using the rotary core barrel (RCB), yielded poor core recovery in the upper 200 mbsf. As a first step in the study of individual core sections from Hole 910D, non-destructive, whole-core X-ray examinations were performed at the Atlantic Geoscience Center of the Bedford Institute of Oceanography in Dartmouth, Nova Scotia, Can-ada. Using a high-resolution video monitor, X-ray images of almost 96 m of core were visually examined and described; these X-ray images were simultaneously recorded on video tape for further digital processing and interpretation. Videotaped X-ray images of the Hole 910D core sections have been used to identify the relative position and size of indi-vidual clasts (>2 mm in diameter) and coarse sand layers, and to identify extensively bioturbated intervals, represented by bur-row traces in these cores. Solid particles>2 mm in diameter, were counted for successive 10-cm intervals of core using the video X-ray images. The X-ray images provide "ground truth " for making comparisons with other nondestructive measure-ments made on these cores using sensors mounted on the multisensor track (MST), and for identifying changes in depositional environments at this site.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Frank R. Rack
Rustan Finndin
Kate Moran
spellingShingle Frank R. Rack
Rustan Finndin
Kate Moran
Background
author_facet Frank R. Rack
Rustan Finndin
Kate Moran
author_sort Frank R. Rack
title Background
title_short Background
title_full Background
title_fullStr Background
title_full_unstemmed Background
title_sort background
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.5488
http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf
long_lat ENVELOPE(-67.150,-67.150,-66.467,-66.467)
ENVELOPE(19.343,19.343,69.775,69.775)
ENVELOPE(5.000,5.000,81.250,81.250)
geographic Bedford
Lier
Yermak Plateau
geographic_facet Bedford
Lier
Yermak Plateau
genre Yermak plateau
genre_facet Yermak plateau
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http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf
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