(Table 1) C, B, and O isotope ratios of sediment samples from ODP Site 180-1114
| Cobertura |
LATITUDE: -9.793550 * LONGITUDE: 151.575067 * DATE/TIME START: 1998-07-12T00:00:00 * DATE/TIME END: 1998-07-16T00:00:00 * MINIMUM DEPTH, sediment/rock: 295.67 m * MAXIMUM DEPTH, sediment/rock: 337.03 m |
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| Data(s) |
23/02/2003
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| Formato |
text/tab-separated-values, 63 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.713252 doi:10.1594/PANGAEA.713252 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.713255 Kopf, Achim J; Behrmann, Jan Hinrich; Deyhle, Annette; Roller, Sybille; Erlenkeuser, Helmut (2003): Isotopic evidence (B, C, O) of deep fluid processes in fault rock from the active Woodlark Basin detachment zone. Earth and Planetary Science Letters, 208(1-2), 51-68, doi:10.1016/S0012-821X(03)00016-5 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #180-1114; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; delta 11B; delta 13C; delta 18O; DEPTH, sediment/rock; ICP-MS, Inductively coupled plasma - mass spectrometry; Joides Resolution; Leg180; Lithology/composition/facies; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Solomon Sea; Temperature, calculated |
| Tipo |
Dataset |
