Mutual replacement reactions in alkali feldspars II: trace element partitioning and geothermometry
Perthitic alkali feldspar primocrysts in layered syenites in the Klokken intrusion in South Greenland, underwent dissolution-reprecipitation reactions in a circulating post-magmatic aqueous fluid at ∼450°C, and are to a large degree pseudomorphs. These
| Main Authors: | , , , , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Springer
2015
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| Subjects: | |
| Online Access: | http://hdl.handle.net/1885/30101 |
| Summary: | Perthitic alkali feldspar primocrysts in layered syenites in the Klokken intrusion in South Greenland, underwent dissolution-reprecipitation reactions in a circulating post-magmatic aqueous fluid at ∼450°C, and are to a large degree pseudomorphs. These |
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