Dolomite/calcite and quartz/calcite ratios of MIS 16 sediments of IODP Site 306-U1313
| Cobertura |
LATITUDE: 41.000000 * LONGITUDE: -32.957300 * DATE/TIME START: 2004-03-28T00:00:00 * DATE/TIME END: 2004-04-02T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.19 m * MAXIMUM DEPTH, sediment/rock: 45.76 m |
|---|---|
| Data(s) |
03/03/2011
|
| Formato |
text/tab-separated-values, 6508 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.757950 doi:10.1594/PANGAEA.757950 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.758056 Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H (2011): Sea surface temperatures did not control the first occurrence of Hudson Strait Heinrich Events during MIS 16. Paleoceanography, 26, PA4201, doi:10.1029/2011PA002135 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #306-U1313; Age model; Age model, optional; COMPCORE; Composite Core; DEPTH, sediment/rock; Dolomite/Calcite ratio; Exp306; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; North Atlantic Climate 2; ODP sample designation; Quartz/Calcite ratio; Sample code/label; Sample code/label 2; X-ray diffraction (XRD) |
| Tipo |
Dataset |
