Unusual exsolution phenomena in omphacite and partial replacement of phengite by phlogopite + kyanite in an eclogite from the Erzgebirge
In the Erzgebirge Crystalline Complex, eclogites occur in three different high pressure (HP) units (1, 2 and 3) recording contrasting pressure (P)-temperature (T) conditions. Eclogites from HP-unit 1 experienced peak metamorphic conditions in the coesite stability field at about 33 kbar/850 degreesC...
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| Veröffentlicht in: | Contributions to mineralogy and petrology 2000-10, Vol.139 (6), p.629-642 |
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| container_title | Contributions to mineralogy and petrology |
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| creator | Schm dicke, Esther M ller, Wolfgang Friedrich |
| description | In the Erzgebirge Crystalline Complex, eclogites occur in three different high pressure (HP) units (1, 2 and 3) recording contrasting pressure (P)-temperature (T) conditions. Eclogites from HP-unit 1 experienced peak metamorphic conditions in the coesite stability field at about 33 kbar/850 degreesC. |
| doi_str_mv | 10.1007/s004100000161 |
| format | Article |
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| ispartof | Contributions to mineralogy and petrology, 2000-10, Vol.139 (6), p.629-642 |
| issn | 0010-7999 1432-0967 |
| language | eng |
| recordid | cdi_proquest_journals_208167150 |
| source | SpringerNature Journals |
| subjects | Geology High pressure Mineralogy Minerals Petrology |
| title | Unusual exsolution phenomena in omphacite and partial replacement of phengite by phlogopite + kyanite in an eclogite from the Erzgebirge |
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