(Table 1) Relative abundance of terrigenous minerals of Hole 302-M0002A
| Cobertura |
LATITUDE: 87.921180 * LONGITUDE: 139.365010 * DATE/TIME START: 2004-08-19T00:00:00 * DATE/TIME END: 2004-08-19T00:00:00 * MINIMUM ORDINAL NUMBER: 1 * MAXIMUM ORDINAL NUMBER: 5 |
|---|---|
| Data(s) |
18/11/2008
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| Formato |
text/tab-separated-values, 265 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.707421 doi:10.1594/PANGAEA.707421 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.707428 Krylov, Alexey A; Andreeva, Irina A; Vogt, Christoph; Backman, Jan; Krupskaya, Viktoria V; Grikurov, Garrik E; Moran, Kathryn; Shoji, Hitoshi (2008): A shift in heavy and clay mineral provenance indicates a middle Miocene onset of a perennial sea ice cover in the Arctic Ocean. Paleoceanography, 23, PA1S06, doi:10.1029/2007PA001497 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #302-M0002A; ACEX-M2A; Apatite; Arctic Coring Expedition, ACEX; Arctic Ocean; Chloritoid; Clinopyroxene; Dolomite; DRILL; Drilling/drill rig; Epidote-zoisite; Exp302; Garnet; Heavy minerals; Hornblende; Indefinite titanium minerals and leucoxene; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Lithologic unit/sequence; Minerals; Number of observations; Optical microscopy; ORDINAL NUMBER; Ore; Ratio; Rock fragments; Rutile; Sphene; Tourmaline; Vidar Viking; Zircon |
| Tipo |
Dataset |
