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TitleBroadband waterborne hammer seismic source for imaging river and lake sub-bottoms
 
AuthorPugin, A J -M; Brewer, K; Brooks, G RORCID logo
SourceSEG19 SEG International Exposition and 89th Annual Meeting; Society of Exploration Geophysicists, Technical Program, Expanded Abstracts 2019, 2019 p. 2750-2754, https://doi.org/10.1190/segam2019-3202612.1
Image
Year2019
Alt SeriesNatural Resources Canada, Contribution Series 20180434
PublisherSociety of Exploration Geophysicists
MeetingSEG19 - SEG International Exposition and 89th Annual Meeting; San Antonio, TX; US; September 15-20, 2019
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceOntario; Quebec
AreaRound Lake; Ottawa River
Subjectsgeophysics; surficial geology/geomorphology; sedimentology; stratigraphy; Science and Technology; Nature and Environment; mapping techniques; geophysical surveys; seismic surveys; in-field instrumentation; glacial deposits; tills; sands; gravels; landslide deposits; mass wasting; buried valleys; depositional history; sedimentation; floods; erosional surfaces; sedimentary structures; faults; alluvial sediments; lacustrine sediments; colluvial and mass-wasting deposits; Data processing; Phanerozoic; Cenozoic; Quaternary
Illustrationsphotographs; seismic profiles; spectra
ProgramPublic Safety Geoscience Eastern Canada Geohazards Assessment Project
Released2019 08 10
Abstract(Summary)
Waterborne surveys were conducted using a handheld hammer hitting a rod attached to an aluminum plate with a single channel hydrophone eel. The broadband signal generated by this recording system produces a data set that can be processed in multiple frequency bands such at 0.5 kHz, 1.5 kHz, 3.5 kHz and 5.5 kHz. The lowest frequency band shows a greater capacity of penetration with reflections observed below high impedance contrasts such as till and sand-gravel layers. The higher frequency bands show the lacustrine sediment layers with greater penetration than that acquired with a 15 kHz CHIRP acoustic profiler system. A survey across Round Lake, Ontario, revealed faulted structures that are interpreted preliminarily to be mass movement-related. A second survey across the Ottawa River, Ontario-Quebec, reveals a buried gorge and a complex sedimentation interpreted as flood-related erosion and deposition.
Summary(Plain Language Summary, not published)
Waterborne surveys were conducted using a carpenter hammer hitting a rod attached to an aluminum plate with a single channel hydrophone eel. The broadband signal generated by this recording system produces a data set that can be processed in multiple frequency bands such at 0.5 kHz, 1.5 kHz, 3.5 kHz and 5.5 kHz. The lowest frequency band shows a greater capacity of penetration with reflections observed below high impedance contrasts such as till and sand-gravel layers. The higher frequency bands show the lacustrine sediment layers with greater penetration than that acquired with a 15 kHz CHIRP acoustic profiler system. A survey across Round Lake, Ontario, revealed faulted structures that are interpreted preliminarily to be mass movement-related. A second survey across the Ottawa River, Ontario-Quebec, reveals a buried gorge and a complex sedimentation interpreted as flood-related erosion and deposition.
GEOSCAN ID314530

 
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