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| 02284nam 2200397zi 4500 |
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001 | 9.912500 |
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003 | CaOODSP |
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005 | 20230131161140 |
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006 | m o d f |
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007 | cr cn||||||||| |
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008 | 220620t20222022nscabd ob f000 0 eng d |
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020 | |a9780660441542 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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043 | |an-cn-ns |
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086 | 1 |aM183-2/8637E-PDF |
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100 | 1 |aJenner, Kimberley-Anne, |d1959- |eauthor. |
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245 | 10|aPiston cores and supporting high-resolution seismic data, CCGS Hudson Expedition 2015018, Scotian Slope, offshore Nova Scotia, Canada / |cK.A. Jenner, D.C. Campbell, J.M. Barnett, J. Higgins, and A. Normandeau. |
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264 | 1|aDartmouth, Nova Scotia : |bGeological Survey of Canada, |c2022. |
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264 | 4|c©2022 |
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300 | |a1 online resource (167 pages) : |billustrations, maps, graphs. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aOpen file, |x2816-7155 ; |v8637 |
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504 | |aIncludes bibliographical references (pages 47-49). |
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520 | |a"The twenty-six piston cores presented in this study were collected during CCGS Hudson cruise 2015018, to the Scotian Slope, between the eastern edge of Northeast Channel and the eastern edge of Logan Canyon, extending from the shelf break to the continental rise, in water depths ranging from 1520 m to 2648 m. The piston cores were collected as part of a joint mission between the Geological Survey of Canada (GSC) and the Nova Scotia Department of Energy (NSDE) to investigate and sample seabed hydrocarbon seep features along the continental slope of Nova Scotia"--Introduction, page 9. |
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650 | 0|aSpectrophotometry|zNova Scotia. |
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650 | 0|aMarine sediments|zNova Scotia. |
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650 | 0|aHydrocarbons|zNova Scotia. |
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650 | 6|aSpectrophotométrie|zNouvelle-Écosse. |
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650 | 6|aSédiments marins|zNouvelle-Écosse. |
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650 | 6|aHydrocarbures|zNouvelle-Écosse. |
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710 | 2 |aGeological Survey of Canada, |eissuing body. |
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830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v8637.|w(CaOODSP)9.506878 |
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856 | 40|qPDF|s231.01 MB|uhttps://publications.gc.ca/collections/collection_2022/rncan-nrcan/m183-2/M183-2-8637-eng.pdf |
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856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/330088 |
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