Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ...
Albian turbidites and intercalated shales were cored from ~1145 to 1700 meters below seafloor at Site 1276 in the Newfoundland Basin. Strata at this level dip ~2.5° seaward (toward an azimuth of ~130°) based on seismic profiles. In contrast, beds dip an average of ~10° in the cores. This higher appa...
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ftdatacite:10.1594/pangaea.776586 2024-09-30T14:38:51+00:00 Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... Hiscott, Richard N 2007 application/zip https://dx.doi.org/10.1594/pangaea.776586 https://doi.pangaea.de/10.1594/PANGAEA.776586 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.210.103.2007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.77658610.2973/odp.proc.sr.210.103.2007 2024-09-02T08:36:09Z Albian turbidites and intercalated shales were cored from ~1145 to 1700 meters below seafloor at Site 1276 in the Newfoundland Basin. Strata at this level dip ~2.5° seaward (toward an azimuth of ~130°) based on seismic profiles. In contrast, beds dip an average of ~10° in the cores. This higher apparent dip is the sum of the ~2.5° seaward dip and a measured hole deviation of 7.43°, which must be essentially in the same seaward direction. Using the maximum dip direction in the cores as a reference direction, paleocurrents were measured from 11 current-ripple foresets and 11 vector means of grain fabric in planar-laminated sandstones. Five of the planar-laminated sandstone samples have a grain imbrication 8°, permitting specification of a unique flow direction rather than just the line-of-motion of the current. Both ripples and grain fabric point to unconfined flow toward the north-northeast. There is considerable spread in the data so that some paleoflow indicators point toward the northwest, whereas others ... : Supplement to: Hiscott, Richard N (2007): Paleoflow directions of Albian basin-floor turbidity currents in the Newfoundland Basin. In: Tucholke, B.E., Sibuet, J.-C., and Klaus, A. (Eds.), Proc. ODP, Sci. Results, 210 : College Station, TX (Ocean Drilling Program), 210, 1-27 ... Article in Journal/Newspaper Newfoundland DataCite Klaus ENVELOPE(24.117,24.117,65.717,65.717) |
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Open Polar |
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ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP |
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Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP Hiscott, Richard N Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
topic_facet |
Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP |
description |
Albian turbidites and intercalated shales were cored from ~1145 to 1700 meters below seafloor at Site 1276 in the Newfoundland Basin. Strata at this level dip ~2.5° seaward (toward an azimuth of ~130°) based on seismic profiles. In contrast, beds dip an average of ~10° in the cores. This higher apparent dip is the sum of the ~2.5° seaward dip and a measured hole deviation of 7.43°, which must be essentially in the same seaward direction. Using the maximum dip direction in the cores as a reference direction, paleocurrents were measured from 11 current-ripple foresets and 11 vector means of grain fabric in planar-laminated sandstones. Five of the planar-laminated sandstone samples have a grain imbrication 8°, permitting specification of a unique flow direction rather than just the line-of-motion of the current. Both ripples and grain fabric point to unconfined flow toward the north-northeast. There is considerable spread in the data so that some paleoflow indicators point toward the northwest, whereas others ... : Supplement to: Hiscott, Richard N (2007): Paleoflow directions of Albian basin-floor turbidity currents in the Newfoundland Basin. In: Tucholke, B.E., Sibuet, J.-C., and Klaus, A. (Eds.), Proc. ODP, Sci. Results, 210 : College Station, TX (Ocean Drilling Program), 210, 1-27 ... |
format |
Article in Journal/Newspaper |
author |
Hiscott, Richard N |
author_facet |
Hiscott, Richard N |
author_sort |
Hiscott, Richard N |
title |
Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
title_short |
Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
title_full |
Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
title_fullStr |
Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
title_full_unstemmed |
Ripple migration directions and grain fabric measurements on ODP Hole 210-1276A sediments ... |
title_sort |
ripple migration directions and grain fabric measurements on odp hole 210-1276a sediments ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.776586 https://doi.pangaea.de/10.1594/PANGAEA.776586 |
long_lat |
ENVELOPE(24.117,24.117,65.717,65.717) |
geographic |
Klaus |
geographic_facet |
Klaus |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.210.103.2007 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.77658610.2973/odp.proc.sr.210.103.2007 |
_version_ |
1811641455727345664 |