Five thin polished sections from brecciated and unbrecciated masses were examined. The unbrecciated specimen is composed of medium gray colored lithology and shows some scattered, faint, texturally equilibrated chondrules set within a recrystallized groundmass. The mean visible chondrule diameter is 0.5mm. The main phases are olivine and orthopyroxene. Olivine shows mosaicism, planar fractures and darkening. Small and rare feldspar grains are present and show undulatory extinction. Opaque phases include metals (kamacite, taenite) and troilite. Other accessory phases include phosphate and chromite. The brecciated lithology consists of a chondritic texture with medium-gray chondritic clasts in a dark-gray chondritic host that has similar texture and composition, but much darker in color. Plagioclase grains are present with sizes up to 50 microns in diameter. Highly recrystallized fragments (type 6) coexist with areas showing a chondritic texture (type 5) and fragments of impact darkening. No melt pockets or veins are present. Olivine shows weak mosaicism and darkening indicating shock stage S4. Kamacite is predominantly found in single crystals with well-defined and distorted Neumann lines.Troilite shows multiple twinning also indicating a shock stage S4.