abstract
- Support is request to assist MS student Erica Serna to test the hypothesis that the BIFs formed under anoxic conditions as a mixture of Fe-Mn oxyhydroxides and minor clays.
Fe isotope biosignatures and the redox state of the ocean recorded in 1.69 Ga late Paleoproterozoic Banded Iron Formations and implications for space exploration
Grant
Overview
date/time interval
- July 2013 - November 2014
awarded by
Affiliation
contributor
- Adriana Heimann Rios Principal Investigator