Portales Valley: A meteoritic sample of the brecciated and metal-veined floor of an impact crater on an H-chondrite asteroid

A shower of meteorite fragments fell at similar to 0730 h local time on 199 8 June 13 near the town of Portales, New Mexico. Thus far, 51 pieces of the Portales Valley (H6) meteorite have been recovered. This meteorite has an unusually large number of metallic veins. Some of these veins are also unus ually thick, having widths on the order of centimeters. These wide veins ha ve fine Widmanstatten structure, which is the first time it has been seen i n an ordinary chondrite. This structure indicates the metallic veins and th e host chondrite cooled slowly. These veins appear to have been produced by shock-metamorphic processes, which we infer produced a >20 km diameter imp act crater on an H-chondrite planetesimal.