There is troilite interstitial. So interesting kamacite particle in unclassified NWA, H-chondrite.

A unique Meteorite to add to your collection.

The certificate presents a chondritic texture, with diffuse chondrules up to 0.05 mm and some up to 1.2 mm in diameter.

Chondrules are porphyry of pyroxene, and barred mainly of olivine. The matrix is recrystallized, and there is a second lithology of completely recrystallized rock, strongly shocked, without chondrules. Metallic phase occupies up to 20% of the volume. There is troilite and iron oxides.

For all these reasons, the analyzed sample for their characterization and analysis have yielded

POSITIVE results in its compatibility for meteorites, being in this case and ordinary chondrite, type H4 {based on XRF data, diameter of chondrules and Fe content}, with a shock degree S3-4 (based on irregular fractures in crystals, planar deformation and stage of iron) and with a weathering degree W3 (based on iron oxidation and silicates alteration).

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