UDEI STATION


Iron, IAB complex, Udei Station grouplet
standby for udei station photo
Fell spring 1927
7° 57' N., 8° 5' E.

A 103 kg mass was seen and heard to fall in the daytime near the Benue River in Nigeria. The Geological Survey of Nigeria learned of the event in 1935 when the mass was recovered from a shallow hole six miles west of the railway station at Udei and 23 miles north of Makurdi. Some reports state that a second mass exists.

The IAB iron-meteorite complex, recently proposed by Wasson and Kallemeyn (2002), comprises iron meteorites from the former IAB-IIICD group, as well as numerous related irons. Many of the members contain silicate inclusions with roughly chondritic compositions. Udei Station is a low-Au member of the IAB complex that is closely related to the main group. On a Ni–Au diagram, a grouplet of six members has been resolved in an area close to the sLL subgroup, but with anomalous Ni contents; these meteorites were designated the Udei Station grouplet. Although theories of formation for these irons commonly attribute their origin to impact-melt pools, correlations between Ni abundance and several chemical and physical properties alternatively suggest an interaction with a crystallizing metallic core. The absolute I–Xe retention age, relative to the Shallowater standard, was calculated to be ~4.558 b.y., while the metamorphic resetting of the K–Ar chronometer occurred ~4.31 b.y. ago (Bogard et al, 2005; Pravdivtseva et al, 2013).

Udei Station is a medium octahedrite that contains a high proportion of silicates and troilite. Silicate inclusions range in size from single grains to as large as 8 cm, and they are composed of enstatite, olivine, oligoclase, and diopside representing various subchondritic rock types including basalt–gabbro, feldspathic orthopyroxenite, lherzolite, and harzburgite. Some of the inclusions crystallized from a low degree partial melt (~3–10%) reaching a peak temperature of <1180°C, while others represent a partial melt residue (Ruzicka and Hutson, 2009). Identification of an FeO-poor, Na-rich gabbroic inclusion similar to one found in Caddo County is only the second discovery of such material. It was concluded that interstitial silicate melt migration and removal occurred, assisted by CO gas (now manifest as graphite), while low abundances of metallic melt (~37%) became trapped in veins between solid silicate assemblages (Ruzicka and Hutson, 2009). One plausible model involves impact processing within small melt pools that led to brecciation and mixing of rock clasts from different locations having different thermal histories (ranging from igneous to chondritic) with metallic melt. These melt pools were then slowly cooled, consistent with burial within a deep regolith.

A formation model which accounts for such a wide variety of inclusions and disparate petrographic evidence was proposed by Ruzicka and Hutson (2009) and Ruzicka (2014). They conceive of a major collisional disruption/jumbling of a partially molten, incompletely differentiated planetesimal. They consider winonaites to be derived from the outer layers of this body. At the same time, they envision the IAB complex irons that were more rapidly cooled, exhibit older I–Xe ages, and which are Ni-rich, to have derived from the middle layers, while those that were more slowly cooled, exhibit younger I–Xe ages, and which are Ni-poor, to have derived from the lowest layers. This was a severe impact that mixed material from different depths on the parent body—solid subchondritic material from the cooler regions, and fractionated material from very hot regions—causing metallic melt to be injected into the silicates.

Udei Station has a Cl–Ar-based CRE age of 123 m.y. (Albrecht et al., 2000). It plots as an anomalous member of group IAB in several regards. It contains a clast best described as a peridotite, composed of the most Fe-rich mafic minerals found among IAB irons. Some variability in appearance is apparent in some members of this grouplet, as can be seen in the Four Corners meteorite. The specimen shown above is a 26.3 g partial slice exhibiting a high content of silicates.