Clay mineral composition and biogenic opal content in upper Miocene to Quaternary drift sediments, ODP Site 178-1095


Autoria(s): Hillenbrand, Claus-Dieter; Ehrmann, Werner
Cobertura

LATITUDE: -66.985400 * LONGITUDE: -78.487867 * DATE/TIME START: 1998-02-13T00:00:00 * DATE/TIME END: 1998-02-13T00:00:00 * MINIMUM DEPTH, sediment/rock: 1.04 m * MAXIMUM DEPTH, sediment/rock: 561.60 m

Data(s)

15/11/2005

Formato

text/tab-separated-values, 3782 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.218251

doi:10.1594/PANGAEA.218251

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.735191

Hillenbrand, Claus-Dieter; Ehrmann, Werner (2005): Late Neogene to Quaternary environmental changes in the Antarctic Peninsula region: evidence from drift sediments. Global and Planetary Change, 45, 165-191, doi:10.1016/j.gloplacha.2004.09.006

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #178-1095; Age model; Calculated, see reference(s); Chlorite; COMPCORE; Composite Core; Depth, composite; DEPTH, sediment/rock; Grain size, sieving/settling tube; Illite; Intercore correlation; interpolated; Joides Resolution; Kaolinite; Leg178; Lithogenic material; Ocean Drilling Program; ODP; ODP sample designation; Opal, auto analysis (Müller & Schneider, 1993); Opal, biogenic silica; Sample code/label; Sedimentation rate; Size fraction < 0.002 mm, > 9 phi, clay; Smectite; South Pacific Ocean; X-ray diffraction TEXTUR, clay fraction
Tipo

Dataset