Spectral and Geochemical Characteristics of Lake Superior Type Banded Iron Formation: Analog to the Martian Hematite Outcrops

Details Spectral and Geochemical Characteristics of Lake Superior Type Banded Iron Formation: Analog to the Martian Hematite Outcrops Spectral and Geochemical Characteristics of Lake Superior Type Banded Iron Formation: Analog to the Martian Hematite Outcrops

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1176f&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1176

Computer Science

Scientific paper

Samples of oxide, carbonate, and silicate facies BIF are measured for
their reflectance (0.4 to 2.5 µm), and emittance (5 to 50
µm). The minerals comprising these facies are possible auxiliary
minerals to the hematite regions on Mars.

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