Age model of IODP Site 339-U1387


Autoria(s): Bahr, André; Jiménez-Espejo, Francisco J; Kolasinac, Nada; Grunert, Patrick; Hernandéz-Molina, Francisco Javier; Röhl, Ursula; Voelker, Antje HL; Escutia, Carlota; Stow, Dorrik A V; Alvarez Zarikian, Carlos A; Hodell, David A
Cobertura

LATITUDE: 36.805000 * LONGITUDE: -7.718000 * MINIMUM DEPTH, sediment/rock: 1.80 m * MAXIMUM DEPTH, sediment/rock: 33.58 m

Data(s)

25/03/2014

Formato

text/tab-separated-values, 32 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.830945

doi:10.1594/PANGAEA.830945

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.831133

Bahr, André; Jiménez-Espejo, Francisco J; Kolasinac, Nada; Grunert, Patrick; Hernandéz-Molina, Francisco Javier; Röhl, Ursula; Voelker, Antje HL; Escutia, Carlota; Stow, Dorrik A V; Alvarez Zarikian, Carlos A; Hodell, David A (2014): Deciphering bottom current strength and paleoclimate signals from contourite deposits in the Gulf of Cádiz during the last 140 kyr: an inorganic geochemical approach. Geochemistry, Geophysics, Geosystems, 15(8), 3145-3160, doi:10.1002/2014GC005356

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #339-U1387; Age model; COMPCORE; Composite Core; DEPTH, sediment/rock; Exp339; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mediterranean Outflow
Tipo

Dataset