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| 02111cam 2200361zi 4500 |
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| 001 | 9.898322 |
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| 003 | CaOODSP |
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| 005 | 20221107174817 |
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| 006 | m o d f |
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| 007 | cr cn||||||||| |
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| 008 | 210407t20192019oncabd o f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn-nf |
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| 086 | 1 |aM183-2/8497E-PDF |
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| 100 | 1 |aMosher, D. |q(David)|eauthor. |
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| 245 | 10|aUltra-high-resolution imaging of submarine landslides : |bthe Geoforce Group Limited Boomer and/or sparker subbottom profiler / |cD.C. Mosher, G. Standen, and D.C. Campbell. |
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| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2019. |
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| 264 | 4|c©2019 |
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| 300 | |a1 online resource (1 unnumbered page) : |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 ; |v8497 |
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| 500 | |aCaption title. |
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| 520 | |a"An ideal subbottom profiler has a broad frequency band, high energy, rapid trigger rate, and highly repeatable source characteristics. These elements provide for maximum vertical and horizontal resolving capacity, subbottom penetration even in hard and gas-bearing sediments, shot-to-shot coherency and phase and amplitude information to facilitate interpretation. In addition, directional source characteristics limit incidental environmental noise. The Geoforce DTS optimizes these characteristics to the physical limits of modern technologies, utilizing two modes of operation: sparker and boomer"--Page [1]. |
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| 650 | 0|aMarine sediments|zScotian Shelf. |
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| 650 | 0|aBottom water (Oceanography)|zScotian Shelf. |
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| 650 | 6|aSédiments marins|zNéo-écossaise, Plateforme. |
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| 650 | 6|aEau de fond (Océanographie)|zNéo-écossaise, Plateforme. |
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| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
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| 830 | #0|aOpen file (Geological Survey of Canada)|v8497.|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s137.76 MB|uhttps://publications.gc.ca/collections/collection_2021/rncan-nrcan/m183-2/M183-2-8497-eng.pdf |
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| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/313251 |
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