(Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core


Autoria(s): O'Regan, Matthew; King, John W; Backman, Jan; Jakobsson, Martin; Pälike, Heiko; Moran, Kathryn; Heil, Chip; Sakamoto, Tatsuhiko; Cronin, Thomas M; Jordan, Richard William
Cobertura

LATITUDE: 87.890000 * LONGITUDE: 137.650000 * MINIMUM DEPTH, sediment/rock: 16.23 m * MAXIMUM DEPTH, sediment/rock: 26.69 m

Data(s)

09/05/2008

Formato

text/tab-separated-values, 28 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.832425

doi:10.1594/PANGAEA.832425

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.832427

O'Regan, Matthew; King, John W; Backman, Jan; Jakobsson, Martin; Pälike, Heiko; Moran, Kathryn; Heil, Chip; Sakamoto, Tatsuhiko; Cronin, Thomas M; Jordan, Richard William (2008): Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography, 23(1), PA1S19, doi:10.1029/2007PA001551

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #302-CompSite; Age model; Arctic Coring Expedition, ACEX; COMPCORE; Composite Core; Datum level; DEPTH, sediment/rock; Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Vidar Viking
Tipo

Dataset