Geochemistry of IODP Site 321-U1338
| Cobertura |
LATITUDE: 2.507800 * LONGITUDE: -117.969910 * MINIMUM DEPTH, sediment/rock: 307.65 m * MAXIMUM DEPTH, sediment/rock: 395.44 m |
|---|---|
| Data(s) |
07/10/2014
|
| Formato |
text/tab-separated-values, 32193 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.820094 doi:10.1594/PANGAEA.820094 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.820095 Holbourn, Ann; Kuhnt, Wolfgang; Lyle, Mitchell W; Schneider, Leah; Romero, Oscar E; Andersen, Nils (2014): Middle Miocene climate cooling linked to intensification of eastern equatorial Pacific upwelling. Geology, 42(1), 19-22, doi:10.1130/G34890.1 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #-; 321-U1338; AGE; Calcium (peak area); Calcium carbonate; Calculated; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Estimated; Exp321; Integrated Ocean Drilling Program / International Ocean Discovery Program; Intercore correlation; IODP; Joides Resolution; log-Silicon/Titanium ratio; log-Titanium/Calcium ratio; ODP sample designation; Pacific Equatorial Age Transect II / Juan de Fuca; Sample code/label; Silicon (peak area); Titanium (peak area); X-ray fluorescence (XRF) |
| Tipo |
Dataset |
