| Locality type: | Deposit |
| Classification |
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| Species: | Crandallite |
| Formula: | CaAl3(PO4)(PO3OH)(OH)6 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Crandallite data |
| Locality Data: | Click here to view Kara-Tangi U deposit, Batken Region, Kyrgyzstan |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 389196 |
| Long-form Identifier: | 1:3:389196:4 |
| GUID (UUID V4): | f4b4879b-4c5b-433e-87d1-e171630cfe6b |
| References |
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Uvarova, Y. A., Sokolova, E., Hawthorne, F. C., Karpenko, V. V., Agakhanov, A. A., Pautov, L. A. (2005) The crystal chemistry of the "nickelalumite"–group minerals. The Canadian Mineralogist, 43 (5) 1511-1519 doi:10.2113/gscanmin.43.5.1511 |
| Reference Search (possible matching items) |
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 | | Book (volume) | | group uramarsite discovered in the Bota-Burum U deposit, Southern Kazakhstan, was detected by characteristic...cm1 is called the fingerprint region. Usually IR spectrum in this region contains very complicated series...overlapping bands. The importance of the fingerprint region is that each mineral species produces a different...500 to 800 cm1 can be considered as “fingerprint region” sensitive to the composition and the topological...see Fig. 1.9), but generally IR spectrum in this region is characteristic of all these minerals. In IR |
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