(Table 1) Silicate oxygen isotope ratios of amphibolite and serpentine from ODP Site 173-1070
| Cobertura |
LATITUDE: 40.796300 * LONGITUDE: -12.723833 * DATE/TIME START: 1997-05-31T00:00:00 * DATE/TIME END: 1997-06-07T00:00:00 * MINIMUM DEPTH, sediment/rock: 659.01 m * MAXIMUM DEPTH, sediment/rock: 717.08 m |
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| Data(s) |
14/01/2000
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| Formato |
text/tab-separated-values, 68 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.711252 doi:10.1594/PANGAEA.711252 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.711255 Skelton, Alsadair SL; Valley, John W (2000): The relative timing of serpentinisation and mantle exhumation at the ocean-continent transition, Iberia: constraints from oxygen isotopes. Earth and Planetary Science Letters, 178(3-4), 327-338, doi:10.1016/S0012-821X(00)00087-X |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #173-1070; COMPCORE; Composite Core; delta 18O; DEPTH, sediment/rock; Joides Resolution; Leg173; Mass spectrometer Finnigan MAT 251; North Atlantic Ocean; Ocean Drilling Program; ODP; Sample comment |
| Tipo |
Dataset |
