Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron

Details Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28.1093p&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 093.

Computer Science

Iron Meteorites, Mineralogy, Group 4A Compounds, Sulfides, Meteoritic Composition, Widmanstatten Structure, Metal Compounds, Minerals, Brasses

Scientific paper

It is suggested on the basis of a study of the mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron that the brassy mineral assemblage was formed in situ due to the invasion of gaseous sulfur along grain boundaries and cracks, and due to the reaction between sulfur and kamacite in the presence of daubreelite at low temperatures. Such a mechanism would account for textures and mineral composites of the brassy masses in a way consistent with low-temperature phase relations in the Fe-Cr-S and Fe-Ni-S systems.

Affiliated with

Also associated with

No associations

Rating

Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Mineralogy and origin of brassy, sulfide-rich masses in the Gibeon IVA iron will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-873787