(Table 7) Oxygen isotope ratio and calculated mineral formation temperature of clay and quartz samples from ODP Hole 193-1189B
| Cobertura |
LATITUDE: -3.720600 * LONGITUDE: 151.675100 * DATE/TIME START: 2000-12-22T07:45:00 * DATE/TIME END: 2000-12-26T17:00:00 * MINIMUM DEPTH, sediment/rock: 40.20 m * MAXIMUM DEPTH, sediment/rock: 196.82 m |
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| Data(s) |
16/12/2004
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| Formato |
text/tab-separated-values, 30 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.710753 doi:10.1594/PANGAEA.710753 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.710756 Lackschewitz, Klas S; Devey, Colin W; Stoffers, Peter; Botz, Reiner; Eisenhauer, Anton; Kummetz, M; Schmidt, Mark; Singer, A (2004): Mineralogical, geochemical and isotopic characteristics of hydrothermal alteration processes in the active, submarine, felsic-hosted PACMANUS field, Manus Basin, Papua New Guinea. Geochimica et Cosmochimica Acta, 68(21), 4405-4427, doi:10.1016/j.gca.2004.04.016 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #193-1189B; Bismarck Sea; Calculated; delta 18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg193; Mass spectrometer Finnigan MAT 251; Minerals; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Temperature, calculated |
| Tipo |
Dataset |
