The Iron Isotopic Composition of 3.7-3.8 Ga Chemical Sediments: Comparison Between Isua (Greenland) and Nuvvuagittuq (Northen Quebec)

Details The Iron Isotopic Composition of 3.7-3.8 Ga Chemical Sediments: Comparison Between Isua (Greenland) and Nuvvuagittuq (Northen Quebec) The Iron Isotopic Composition of 3.7-3.8 Ga Chemical Sediments: Comparison Between Isua (Greenland) and Nuvvuagittuq (Northen Quebec)

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1053d&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1053

Computer Science

Scientific paper

The BIFs in the 3.7-3.8 Ga Nuvvuagittuq Belt have heavy Fe isotopic
compositions, similar to those measured in the better-characterized Isua
Supracrustal Belt. This is the first time in 40 years that an early
Archean supracrustal belt has been opened up for study.

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