The pseudometeorite Angara

Holger Pedersen

Abstract

Several pallasites are known to have formed strewn fields with multiple fragments. Therefore, it seems possible that the famous Krasnojarsk pallasite-the Pallas Iron of 687 kg-could have been accompanied by one or more additional fragments that had not been recovered due to incomplete observations from the overgrown and remote place of fall. During a survey for literature accounts of distant fragments in such a hypothetical strewn field, a report of native iron was found, dating to 1847. The fragments of nickel-free iron-amounting to at least a few kg-had been recovered 1836-1843 during placer gold mining north of the Angara River. The position of these finds is coincident with Burovaya, Murozhna, and Uderei, the three known fragments of the pseudometeorite Angara, all collected in 1885.

OriginalsprogEngelsk
TidsskriftMeteoritics and Planetary Science
Vol/bind48
Udgave nummer6
Sider (fra-til)1091-1095
ISSN1086-9379
DOI
StatusUdgivet - 1 jun. 2013

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