Krastel, Sebastian; Bräunig, Anja; Feldens, Peter; Georgiopoulou, Aggeliki; Jähmlich, Heiko; Lange, Matthias; Lindhorst, Katja; Llopart, Jaume; Mader, Sarah; Mehringer, Lisa; Merl, Maximilian; Mücke, Isabell; Renkl, Christoph; Roskoden, Robert; Schönke, Mischa; Schulten, Irena; Schwarz, Jan-Philipp; Stevenson, Christopher; Vallee, Maxlimer; Wegener, Babette; Wiesenberg, Lars (2019): Sediment echo sounding during Maria S. Merian cruise MSM47 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.907945, In: Krastel, S et al. (2019): The 1929 Grand Banks landslide of the Canadian Atlantic continental margin - Cruise No. MSM47 - September 30 - October 30, 2015 - St. John's (Canada) - Ponta Delgada, Azores (Portugal). Bathymetry and subsurface based on seismic, acoustic and core data [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.907950
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
.SGY files were recorded with the onboard parasound system. The Atlas PARASOUND system P70 uses the parametric effect, which occurs when very high (finite) amplitude sound waves are generated. If two waves of similar frequencies are generated simultaneously, also the sum and the difference of the two primary frequencies are emitted. For the PARASOUND System, 18 kHz is one fixed primary frequency, which is generated by a transducer of ~ 1m length within a beam of 4.5°. The second primary frequency can be varied between 18.5 and 24 kHz, resulting in difference frequencies from 0.5 to 6.0 kHz. The system treats three signals separately: the primary high frequency signal (18 kHz; PHF), the secondary low frequency signal (selectable 0.5 to 6.0 kHz; SLF) and the secondary high frequency (selectable 36.5 to 42 kHz; SHF). We selected 4 kHz as SLF and 40 kHz as SHF. The segy files attached here represent the SLF signal.
Related to:
Stevenson, Christopher; Feldens, Peter; Georgiopoulou, Aggeliki; Schönke, Mischa; Krastel, Sebastian; Piper, David J W; Lindhorst, Katja; Mosher, David C (2018): Reconstructing the sediment concentration of a giant submarine gravity flow. Nature Communications, 9(1), https://doi.org/10.1038/s41467-018-05042-6
Coverage:
Median Latitude: 42.646500 * Median Longitude: -39.184000 * South-bound Latitude: 37.735000 * West-bound Longitude: -52.705000 * North-bound Latitude: 47.558000 * East-bound Longitude: -25.663000
Event(s):
MSM47-track * Latitude Start: 47.558000 * Longitude Start: -52.705000 * Latitude End: 37.735000 * Longitude End: -25.663000 * Campaign: MSM47 * Basis: Maria S. Merian * Method/Device: Underway cruise track measurements (CT)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | File name | File name | Feldens, Peter | |||
2 | File format | File format | Feldens, Peter | |||
3 | File size | File size | kByte | Feldens, Peter | ||
4 | Uniform resource locator/link to sgy data file | URL sgy | Feldens, Peter |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
892 data points