(Table 1) Sr and Nd istopic ratios for ODP Leg 134 volcanics and volcaniclastics
| Cobertura |
MEDIAN LATITUDE: -15.238250 * MEDIAN LONGITUDE: 167.123500 * SOUTH-BOUND LATITUDE: -16.009000 * WEST-BOUND LONGITUDE: 166.284000 * NORTH-BOUND LATITUDE: -14.796000 * EAST-BOUND LONGITUDE: 167.880000 * DATE/TIME START: 1990-10-25T11:00:00 * DATE/TIME END: 1990-12-14T00:30:00 * MINIMUM DEPTH, sediment/rock: 0.260 m * MAXIMUM DEPTH, sediment/rock: 1097.100 m |
|---|---|
| Data(s) |
21/08/1994
|
| Formato |
text/tab-separated-values, 164 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.787571 doi:10.1594/PANGAEA.787571 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.787578 Briqueu, Louis; Laporte, C; Crawford, Anthony J; Hasenaka, Toshiaki; Baker, Peter E; Coltorti, Massimo (1994): Temporal magmatic evolution of the Aoba Basin, Central New Hebrides Island Arc: Pb, Sr, and Nd isotopic evidence for the coexistence of two mantle components beneath the Arc. In: Green, HG; Collot, J-Y; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 134, 393-401, doi:10.2973/odp.proc.sr.134.019.1994 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #134-828A; 134-829A; 134-830B; 134-831B; 134-832A; 134-832B; 134-833A; 134-833B; Coral Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Latitude of event; Leg134; Lithologic unit/sequence; Longitude of event; Neodymium 143/Neodymium 144; Neodymium 143/Neodymium 144, error; Ocean Drilling Program; ODP; ODP sample designation; Optional event label; Sample code/label; Strontium 87/Strontium 86, error; Strontium 87/Strontium 86 ratio |
| Tipo |
Dataset |
