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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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) |
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Open Polar |
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ftciteseerx |
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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. |
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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 |
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Background |
title_fullStr |
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title_full_unstemmed |
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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 |
op_source |
http://www-odp.tamu.edu/publications/151_SR/VOLUME/CHAPTERS/sr151_21.pdf |
op_relation |
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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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766236937258008576 |