(Table 1) Sediment characteristics at DSDP Hole 75-532A
| Cobertura |
LATITUDE: -19.744000 * LONGITUDE: 10.518800 * DATE/TIME START: 1980-08-20T00:00:00 * DATE/TIME END: 1980-08-20T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.17 m * MAXIMUM DEPTH, sediment/rock: 198.72 m |
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| Data(s) |
16/04/1984
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| Resumo |
Orientation and geometry of pores as well as sediment compressibility can be approximated by determining the shrinkage behavior of standardized samples. The sections investigated show that these measurements are influenced by changing sediment composition. This is also well documented by the relationship between void ratio and overburden pressure. Median pore-diameter calculations clearly reflect both sediment composition and compaction. |
| Formato |
text/tab-separated-values, 798 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.810291 doi:10.1594/PANGAEA.810291 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Wetzel, Andreas (1984): Interrelationships between sediment composition, compaction, pore space, and shrinkage, Leg 75, Hole 532A. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 1129-1136, doi:10.2973/dsdp.proc.75.142.1984 |
| Palavras-Chave | #75-532A; Areameter; Calculated, see reference(s); Carbonates; Deep Sea Drilling Project; Density, wet bulk; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg75; Loss; ODP sample designation; Pore radius, mean; Porosity, fractional; Sample code/label; see reference(s); Size fraction < 0.002 mm, > 9 phi, clay; Size fraction > 0.063 mm, sand; Size fraction 0.006-0.002 mm; Size fraction 0.020-0.006 mm; Size fraction 0.063-0.020 mm, coarse silt; South Atlantic; Specific surface area; Void ratio; Water content of wet mass; Wet sieving |
| Tipo |
Dataset |
