Hello Elton,

The following excerpt is from my Tombigbee River webpage:

Most specimens in this group [tentatively IIG] have a hexahedrite-like
matrix consisting predominately of kamacite, but one mass lower in P and
higher in Ni shows a small area with a remnant coarse Widmanst�tten
structure. It was proposed by Vagn F. Buchwald that these irons be
structurally classified as hexahedrite, transitional to coarsest
octahedrite (H-Ogg). 

Regards,
David
meteoritestudies.com

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