(Table 1) Magnetic susceptibility and laboratory-imparted magnetization at ODP Hole 133-819A
| Cobertura |
LATITUDE: -16.624000 * LONGITUDE: 146.324700 * DATE/TIME START: 1990-09-10T01:24:00 * DATE/TIME END: 1990-09-12T06:50:00 * MINIMUM DEPTH, sediment/rock: 0.16 m * MAXIMUM DEPTH, sediment/rock: 120.18 m |
|---|---|
| Data(s) |
06/07/1993
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| Formato |
text/tab-separated-values, 4478 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.785596 doi:10.1594/PANGAEA.785596 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.785608 Alexander, Ian T; Kroon, Dick; Thompson, Roy (1993): Late Quaternary paleoenvironmental change on the northeast Australian Margin as evidenced in oxygen isotope stratigraphy, mineral magnetism, and sedimentology. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 129-161, doi:10.2973/odp.proc.sr.133.224.1993 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #133-819A; ARM, Intensity, per unit mass; ARM Susceptibility/susceptibility ratio; Coral Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; IRM, Intensity, per unit mass; Joides Resolution; Leg133; Ocean Drilling Program; ODP; Saturation isothermal remanent magnetisation/kappa ratio; Saturation isothermal remanent magnetization, intensity, per unit mass; S-ratio (Hematite/Magnetite); Susceptibility, specific |
| Tipo |
Dataset |
