(Table 7) Oxygen isotope ratio and calculated mineral formation temperature of clay and quartz samples from ODP Hole 193-1189B


Autoria(s): Lackschewitz, Klas S; Devey, Colin W; Stoffers, Peter; Botz, Reiner; Eisenhauer, Anton; Kummetz, M; Schmidt, Mark; Singer, A
Cobertura

LATITUDE: -3.720600 * LONGITUDE: 151.675100 * DATE/TIME START: 2000-12-22T07:45:00 * DATE/TIME END: 2000-12-26T17:00:00 * MINIMUM DEPTH, sediment/rock: 40.20 m * MAXIMUM DEPTH, sediment/rock: 196.82 m

Data(s)

16/12/2004

Formato

text/tab-separated-values, 30 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.710753

doi:10.1594/PANGAEA.710753

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.710756

Lackschewitz, Klas S; Devey, Colin W; Stoffers, Peter; Botz, Reiner; Eisenhauer, Anton; Kummetz, M; Schmidt, Mark; Singer, A (2004): Mineralogical, geochemical and isotopic characteristics of hydrothermal alteration processes in the active, submarine, felsic-hosted PACMANUS field, Manus Basin, Papua New Guinea. Geochimica et Cosmochimica Acta, 68(21), 4405-4427, doi:10.1016/j.gca.2004.04.016

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Palavras-Chave #193-1189B; Bismarck Sea; Calculated; delta 18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg193; Mass spectrometer Finnigan MAT 251; Minerals; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label; Temperature, calculated
Tipo

Dataset