Structural ordering of carbonaceous matter in Penninic terranes
This paper presents a study of relations between graphitization processes and metamorphic conditions in the easternmost windows of the Alpine Penninic system (Eastern Austria, Western Hungary). Samples for comparison were collected from the Tauern Window, too. From XRD investigations it can be concl...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1989
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| Sorozat: | Acta mineralogica-petrographica
30 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24773 |
| Tartalmi kivonat: | This paper presents a study of relations between graphitization processes and metamorphic conditions in the easternmost windows of the Alpine Penninic system (Eastern Austria, Western Hungary). Samples for comparison were collected from the Tauern Window, too. From XRD investigations it can be concluded that strong shearing could result in development of graphite in greenschist fades conditions. The mobility of metamorphic fluids also plays a determining role in graphitization. |
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| Terjedelem/Fizikai jellemzők: | 103-113 |
| ISSN: | 0365-8066 |