Retrograded eclogite in the crystalline basement of Tisza Unit, Hungary
Crystalline basement of Eastern part of Tisza Unit in Hungary has been said to be built up of amphibolite facies rocks. However, some samples of these contain relics of an earlier high pressure event and sporadically eclogitic remnants also occur. A symplectitic rock from borehole Korosladany-5 incl...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1995
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| Sorozat: | Acta mineralogica-petrographica
36 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24827 |
| Tartalmi kivonat: | Crystalline basement of Eastern part of Tisza Unit in Hungary has been said to be built up of amphibolite facies rocks. However, some samples of these contain relics of an earlier high pressure event and sporadically eclogitic remnants also occur. A symplectitic rock from borehole Korosladany-5 includes garnet fragments (Py = 30%), phengite, rutile and also pseudomorph after alkali pyroxene. These traces corresponding to other mineralogical observations imply a one-time B or C type eclogitic material. |
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| Terjedelem/Fizikai jellemzők: | 117-128 |
| ISSN: | 0365-8066 |