Ronimisele

Ronimisele is a proposed mineral species that was first mentioned in a 1969 scientific paper by geologist A. O. Isachenko. According to Isachenko, Ronimisele is a lead-rich sulfide mineral with a chemical composition of Pb6As2S9. However, the description and properties of Ronimisele are not well-documented, and the validity of this mineral species has been disputed by several researchers.

Isachenko's initial report on Ronimisele was based on observations of a mineral specimen from a gold-silver deposit in Kazakhstan. However, subsequent attempts to verify the existence and characteristics of Ronimisele have been inconclusive.

To date, there is little to no information available on the physical properties, crystal structure, or occurrences of Ronimisele. The IMA, or International Mineralogical Association, maintains a comprehensive database of recognized mineral species, but Ronimisele is not listed as an officially recognized mineral.

Despite the controversy surrounding its existence, Ronimisele has been mentioned in some older scientific literature, particularly those dealing with the geology of Central Asia. However, most researchers have dismissed Ronimisele as an unverified or potentially fictional mineral species.

Due to the lack of reliable information and the absence of a peer-reviewed validation, the existence of Ronimisele remains unconfirmed. As a result, further research is required to determine the validity of this proposed mineral species.