(Table S8) Amphibole-plagioclase thermometry reconstruction for Pito Deep samples
| Cobertura |
MEDIAN LATITUDE: -22.918125 * MEDIAN LONGITUDE: -111.978500 * SOUTH-BOUND LATITUDE: -22.969000 * WEST-BOUND LONGITUDE: -112.069000 * NORTH-BOUND LATITUDE: -22.875000 * EAST-BOUND LONGITUDE: -111.877000 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.00 m |
|---|---|
| Data(s) |
21/05/2008
|
| Formato |
text/tab-separated-values, 108 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.782660 doi:10.1594/PANGAEA.782660 |
| 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; Aluminium oxide; ALVIN; Area/locality; AT11-23; Atlantis (1997); Calcium oxide; Chromium(III) oxide; Depth, bathymetric; Depth, relative; DEPTH, sediment/rock; Electron microprobe; Elements, total; Event label; Iron oxide, FeO; J2-119-3; J2-121-2; J2-122-3; Latitude of event; Longitude of event; Magnesium oxide; Manganese oxide; Occurrence; Potassium oxide; Remote operated vehicle Jason II; ROVJ; Sample code/label; Silicon dioxide; Sodium oxide; Submersible Alvin; Sum; Temperature, calculated; Titanium oxide; Western Pacific |
| Tipo |
Dataset |
