Bulk mineral composition on cores C00018, C0002D, C0002B and C0006E
Cobertura |
MEDIAN LATITUDE: 33.196101 * MEDIAN LONGITUDE: 136.687129 * SOUTH-BOUND LATITUDE: 33.027407 * WEST-BOUND LONGITUDE: 136.636517 * NORTH-BOUND LATITUDE: 33.300125 * EAST-BOUND LONGITUDE: 136.793803 * DATE/TIME START: 2007-12-29T00:00:00 * DATE/TIME END: 2007-12-29T00:00:00 * MINIMUM DEPTH, sediment/rock: 28.415 m * MAXIMUM DEPTH, sediment/rock: 704.675 m |
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Data(s) |
05/03/2014
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Formato |
text/tab-separated-values, 884 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.830315 doi:10.1594/PANGAEA.830315 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.830343 Usman, Muhammed Ojoshogu; Masago, Hideki; Winkler, Wilfried; Strasser, Michael (2014): Mid Quaternary decoupling of sediment routing in the Nankai Forearc revealed by provenance analysis of turbiditic sands. International Journal of Earth Sciences, doi:10.1007/s00531-014-1011-z |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #315-C0002B; 315-C0002D; 316-C0006E; 333-C0018A; Chert; Chikyu; Counting 63-250 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Exp315; Exp316; Exp333; Feldspar; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Kalifeldspar; Lithic grains; Mica; Mica, polycrystalline; NanTroSEIZE Stage 1: Megasplay Riser Pilot; NanTroSEIZE Stage 1: Shallow Megaslay and Frontal Thrusts; NanTroSEIZE Stage 2: Subduction Inputs 2 and Heat Flow; Normalized; Orthoclase; Plagioclase; Plagioclase/Feldspar ratio; Quartz; Quartz, monocrystalline; Quartz, polycrystalline; Quartz, tectonic; Quartz-mica, tectonic; Sample, optional label/labor no; Sample code/label; Sedimentary fragments; Total; Volcanic lithiclasts |
Tipo |
Dataset |