(Table S3) Plagioclase compositions of Pito Deep samples
| Cobertura |
MEDIAN LATITUDE: -22.930072 * MEDIAN LONGITUDE: -111.957586 * SOUTH-BOUND LATITUDE: -22.983000 * WEST-BOUND LONGITUDE: -112.069000 * NORTH-BOUND LATITUDE: -22.873000 * EAST-BOUND LONGITUDE: -111.875000 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m |
|---|---|
| Data(s) |
21/05/2008
|
| Formato |
text/tab-separated-values, 7411 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.782655 doi:10.1594/PANGAEA.782655 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.782661 Heft, Kerri L; Gillis, Kathryn M; Pollock, Meagen A; Karson, Jeffrey A; Klein, Emily M (2008): Role of upwelling hydrothermal fluids in the development of alteration patterns at fast spreading ridges: Evidence from the sheeted dike complex at Pito Deep. Geochemistry, Geophysics, Geosystems, 9, Q05O07, doi:10.1029/2007GC001926 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Al-4075; Al-4076; Al-4077; Al-4079; Al-4081; Al-4082; Al-4083; Al-4084; Al-4086; Aluminium; Aluminium oxide; ALVIN; Anorthite; Area/locality; AT11-23; Atlantis (1997); Calcium; Calcium oxide; Calculated based on oxygen number; Depth, bathymetric; Depth, relative; DEPTH, sediment/rock; Electron microprobe; Elements, total; Event label; Iron 2+ and 3+; Iron oxide, FeO; J2-119-1; J2-119-2; J2-119-3; J2-120-4; J2-121-1; J2-121-2; J2-122-3; J2-123-4; J2-123-5; Latitude of event; Lithology/composition/facies; Longitude of event; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Potassium; Potassium oxide; Remote operated vehicle Jason II; ROVJ; Sample code/label; Silicon; Silicon dioxide; Sodium; Sodium oxide; Submersible Alvin; Titanium; Titanium oxide; Western Pacific |
| Tipo |
Dataset |
