Locality type: Outcrop Classification Species: Taramite Formula: Na(CaNa)(Mg3 Al2 )(Al2 Si6 O22 )(OH)2 Chemical Analyses: Oxide wt%: 1 SiO2 38.52 % TiO2 0.05 % Al2 O3 21.44 % Cr2 O3 0.00 % Fe2 O3 9.29 % FeO 8.65 % MnO 0.11 % MgO 7.13 % CaO 9.29 % Na2 O 3.76 % K2 O 0.00 % H2 O 2.05 % Total: 100.29 %
Sample references: 1 VAN 98-2- 40 OberhÃĪnsli, R., Koralay, E., Candan, O., Pourteau, A., Bousquet, R. (2013) Late Cretaceous eclogitic high-pressure relics in the Bitlis Massif. Geodinamica Acta , 26 (3) 175-190 doi:10.1080/09853111.2013.858951
Comments: In the eclogites, amphiboles occur as amphiboleâbiotite coronas on garnet, as a matrix of amphiboleâplagioclase symplectites and as a replacement of omphacite. Taramite has been identified as one of these amphiboles. Confirmation Validity: Believed Valid Data Mineral Data: Click here to view Taramite data Locality Data: Click here to view Kesandere valley eclogites, Bitlis Province, Turkey Data Identifiers Mindat Occurrence Record ID: 1744140 Long-form Identifier: 1:3:1744140:9 GUID (UUID V4 ): 0 References OberhÃĪnsli, R., Koralay, E., Candan, O., Pourteau, A., Bousquet, R. (2013) Late Cretaceous eclogitic high-pressure relics in the Bitlis Massif. Geodinamica Acta , 26 (3) 175-190 doi:10.1080/09853111.2013.858951 Search for references including Taramite Kesandere valley eclogites, Bitlis Province, Turkey