Hello Rodrigo and list,

Vagn Buchwald's "Handbook of Iron Meteorites" (1976) has a rather detailed 
discussion of nickel content on pages 76-77 with several histograms showing 
the frequency distribution of percentage nickel content. He states, "In 
iron meteorites, nickel varies from a minimum of 5.1-5.3% (Tombigbee River, 
Auburn, Holland's Store) to a maximum of 35% (Santa Catharina). If 
Oktibbeha County, page 947, is confirmed as an independent meteorite, the 
nickel maximum increases to about 60%."

In Buchwald's histograms, the most nickel-poor iron group, the IIA 
hexahedrites, show a bell-shaped distribution which drops off very sharply 
below 5.3%. Of course, Buchwald's data set is now 26 years old and 
meteoritic science has not stood still in the years since his masterpiece 
was published. Still, the only irons which I am aware of with nickel 
content below the 5.1% lower bound which Buchwald claims are the so-called 
Bellsbank trio, which includes Bellsbank, La Primitiva, and Tombigbee 
River. These are classified as chemically and structurally anomalous (UNGR) 
but appear to be related to the IIAB irons. A nickel content of 4.3% was 
determined for Tombigbee River in 1973, a fact which Buchwald was 
apparently unaware of at the time his Handbook was published. A paper 
published in 1984 by Malvin, Zong, and Wasson presents a hypothesis for a 
process which may have allowed the Bellsbank trio to form under very 
exceptional circumstances in isolated pockets of phosphorus-rich melt in 
the IIAB core, with their anomalous composition as a result. This paper is 
available online at http://adsabs.harvard.edu/abstract_service.html (search 
for "Bellsbank").

All things considered, it seems much more likely that an iron specimen with 
nickel content below around 4% is manmade rather than a representative of 
an as yet undiscovered group of iron meteorites. Buchwald points out that 
nickel is extremely siderophile ("iron loving"), even more so than iron 
itself. Processes of fractionation in the metal phase allow for a rather 
wide range of iron/nickel ratios, but the laws of physical chemistry seem 
to draw the line at around 4% as a lower bound.

Best wishes to all,

Piper

Standard disclaimer: I am not now and have never been a professional 
meteoriticist or geochemist, and any personal opinions not supported by 
references to authorities more qualified than myself should be taken with 
the usual grain of salt. 



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