(Table 3) Isotopic composition of pyrite sulfur and carbonate carbon in carbonate nodules and host sediments from Core DM9-666, Gulf of California


Autoria(s): Lein, Alla Yu
Cobertura

LATITUDE: 24.895000 * LONGITUDE: -108.700000 * MINIMUM DEPTH, sediment/rock: 0.25 m * MAXIMUM DEPTH, sediment/rock: 2.75 m

Data(s)

11/07/2004

Resumo

Isotopic-geochemical study revealed presence of mantle He (3He/4He up to 223x10**-8) in gases from mud volcanoes of Eastern Georgia. This fact confirms that the Middle Kura basin fill encloses an intrusive body previously distinguished from geophysical data. Wide variations of carbon isotopic composition d13C in CH4 and CO2 and chemical composition of gas and water at temporally constant 3He/4He ratio indicate their relation with crustal processes. Unusual direct correlations of 3He/4He ratio with concentrations of He and CH4 and 40Ar/36Ar ratio can be explained by generation of gas in the Cenozoic sequence of the Middle Kura basin.

Formato

text/tab-separated-values, 69 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.785873

doi:10.1594/PANGAEA.785873

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.785878

Lein, Alla Yu (2004): Authigenic carbonate formation in the ocean. Translated from Litologiya i Poleznye Iskopaemye, 2004, 1, 3-35, Lithology and Mineral Resources, 39(1), 1-30, http://www.springerlink.com/content/p12u16433521q389/

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow

Palavras-Chave #Archive of Ocean Data; ARCOD; delta 13C; delta 13C, organic carbon; delta 34S, pyrite; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM9; DM9-666; Dmitry Mendeleev; GC; Gravity corer; Mass spectrometry; Radiotracer; Sample type; Sulfate reduction rate, sediment
Tipo

Dataset