Specimen NumberCRC-24CommentsEDS consistent with this phase. However, new mineral dalnegorskite, accepted in 2018, is actually more likely in this instance as true wollastonite has not been documented within the Bor deposit.In Teaching CollectionNoMineral(s)wollastoniteRock NameCrowe reference collectionDistrictDalnegorskMineBorExternal LinkMindatDeposit TypeSkarnGeo-Coords[1] Reference MaterialBezenek, S.R., 1996, Determination of Temporal Fluid Evolution in the Dalnegorsk Hydrothermal System: an Integrated Study of 18O and major Element Fluctuation Within Zoned Garnets; University of Georgia MS thesis, 147 p.
Kane, M., 1996, Petrology and Geochemistry of the Sn-W-B Mesozoic to Cenozoic Granites in Primorye (Far East Russia): Geodynamic Implications; University of Georgia PhD dissertation, 181 p.
Lieth, F.G., 1996, Oxygen Isotope Study of the Dalnegorsk Borosilicate Skarn, Far East Russia, Primorye Region; University of Georgia MS thesis, 105 p.CitationAnalytical work financially supported by the UGA Department of Geology. Mr. Christopher J. Fleisher is acknowledged for providing technological support for EDS analyses.
CRC-24: Crowe reference collection - Dalnegorsk District - Bor Mine. Franklin College Collections, accessed 13/11/2026, https://digitalcollections.franklin.uga.edu/nodes/view/36707