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F., Grenne, T., Bekker, A., 2009, Seafloor-hydrothermal Si-Fe-Mn exhalites in the Pecos greenstone belt, New Mexico, and the redox state of ca.
2.15 Ga Sengoma Argillite Formation, Botswana: Evidence for oxidative continental weathering during the Great Oxidation Event, Chemical Geology, v.
J., Bekker, A., 2009, U-Th-Pb-REE systematics of organic-rich shales from the ca. Pollack et al., 2009Guo, Q., Strauss, H., Kaufman, A. A., Bekker, A., Kim, S.-T., Farquhar, J., 2009, Reconstructing Earth's surface oxidation across the Archean-Proterozoic transition, Geology, v.
Eons are divided into eras, which are in turn divided into periods, epochs and ages.
The following four timelines show the geologic time scale.
Structure and development of a microcontinent; Elan Bank in the southern Indian Ocean, Geochem.