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Weak hydrothermal carbonation of the Ongeluk volcanics: evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation

Research output: Contribution to journal › Article › peer-review

Laboratory for the Evolution of Paleoocean and Mantle Magmatism

DOI

https://doi.org/10.1186/s40645-017-0145-6
Final published version

Takazo Shibuya
Tsuyoshi Komiya
Ken Takai
Shigenori Maruyama
Michael J. Russell

Original language	English
Article number	31
Number of pages	13
Journal	Progress in Earth and Planetary Science
Volume	4
Issue number	1
DOIs	https://doi.org/10.1186/s40645-017-0145-6
Publication status	Published - 23 Oct 2017

Research areas

Paleoproterozoic global glaciation, Ongeluk volcanics, Carbonation, Carbon and oxygen isotopes, Seawater/atmosphere CO2 level, BARBERTON GREENSTONE-BELT, UPPER OCEANIC-CRUST, SOUTH-AFRICA, SNOWBALL EARTH, PILBARA CRATON, ARCHEAN OCEAN, PRECAMBRIAN ATMOSPHERE, ISOTOPIC COMPOSITION, FLOOR METAMORPHISM, WESTERN-AUSTRALIA, Seawater/ atmosphere CO level

OECD FOS+WOS

ID: 18730360