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  • 152; 153; 158; 170; Bush Hill; Center for Marine Environmental Sciences; DAPC; Device type; Dynamic autoclave piston corer; Elevation of event; Event label; Gas hydrate; Gas hydrate volume; Latitude of event; Length; Longitude of event; MAC; MARUM; Methane; Methane, absolute volume; Multi autoclave corer; OTEGA II; see reference(s); SO174/1; SO174/1_118; SO174/1_63; SO174/1_90; SO174/2; SO174/2_152; SO174/2_153; SO174/2_158; SO174/2_170; Sonne  (1)
  • 204-1244; 204-1245; 204-1246; 204-1247; 204-1248; 204-1249; 204-1250; 204-1252; Angle; Clast shape; COMPCORE; Composite Core; Computer tomography (CT) MARCONI Medical MX 8000; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg204; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label  (1)
  • 204-1244C; 204-1244E; 204-1245B; 204-1247B; 204-1248C; 204-1249B; 204-1249C; 204-1249F; 204-1250D; 204-1252A; Angle; Clast shape; Computer tomography (CT) MARCONI Medical MX 8000; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg204; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2023-06-27
    Keywords: 152; 153; 158; 170; Bush Hill; Center for Marine Environmental Sciences; DAPC; Device type; Dynamic autoclave piston corer; Elevation of event; Event label; Gas hydrate; Gas hydrate volume; Latitude of event; Length; Longitude of event; MAC; MARUM; Methane; Methane, absolute volume; Multi autoclave corer; OTEGA II; see reference(s); SO174/1; SO174/1_118; SO174/1_63; SO174/1_90; SO174/2; SO174/2_152; SO174/2_153; SO174/2_158; SO174/2_170; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Abegg, Friedrich; Bohrmann, Gerhard; Kuhs, Werner F (2006): Data report: Shapes and structures of gas hydrates imaged by computed tomographic analyses, ODP Leg 204, Hydrate Ridge. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-11, https://doi.org/10.2973/odp.proc.sr.204.122.2006
    Publication Date: 2024-01-09
    Description: The sediments of Hydrate Ridge/Cascadia margin contain extensive amounts of gas hydrate. A total of 57 sediment samples including gas hydrate were preserved in liquid nitrogen and have been imaged using computerized tomography to visualize hydrate distribution and shape. The analysis gives evidence that gas hydrate in vein and veinlet structures is the predominant shape in the deeper gas hydrate stability zone with dipping angles from 30° to 90°(vertical).
    Keywords: 204-1244; 204-1245; 204-1246; 204-1247; 204-1248; 204-1249; 204-1250; 204-1252; Angle; Clast shape; COMPCORE; Composite Core; Computer tomography (CT) MARCONI Medical MX 8000; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg204; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 160 data points
    Location Call Number Limitation Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Abegg, Friedrich; Bohrmann, Gerhard; Freitag, Johannes; Kuhs, Werner F (2007): Fabric of gas hydrate in sediments from Hydrate Ridge - results from ODP Leg 204 samples. Geo-Marine Letters, 27, 269-277, https://doi.org/10.1007/s00367-007-0080-4
    Publication Date: 2024-01-09
    Description: Drilling on Hydrate Ridge, offshore Oregon, during ODP Leg 204 enabled us to investigate fabrics of gas hydrate samples in a wide depth range of the gas hydrate stability zone (GHSZ). X-ray computerized tomographic imaging on whole-round samples, frozen in liquid nitrogen, revealed that layered gas hydrate structures are related to variable processes occurring at different sediment depths. Shallow gas hydrates often form layers parallel or sub-parallel to bedding and also crosscut sedimentary strata and other gas hydrate layers, destroying the original depositional fabric. The dynamic processes interacting with this complicated plumbing system in this shallow environment are responsible for such highly variable gas hydrate fabrics. Gas hydrate layers deeper in the sediments are most often dipping with various angles, and are interpreted as gas hydrate precipitates filling tectonic fractures. These originally open fractures are potential candidates for free gas transportation, and might explain why free gas can rapidly emanate from below the bottom-simulating reflector through the GHSZ to the seafloor.
    Keywords: 204-1244C; 204-1244E; 204-1245B; 204-1247B; 204-1248C; 204-1249B; 204-1249C; 204-1249F; 204-1250D; 204-1252A; Angle; Clast shape; Computer tomography (CT) MARCONI Medical MX 8000; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg204; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
    Location Call Number Limitation Availability
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