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...

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Elmentve itt :
Bibliográfiai részletek
Szerző: M. Tóth Tivadar
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1995
Sorozat:Acta mineralogica-petrographica 36
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24827
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490 0 |a Acta mineralogica-petrographica  |v 36 
520 3 |a 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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695 |a Kőzettan, Ásványtan, Földtan 
856 4 0 |u http://acta.bibl.u-szeged.hu/24827/1/mineralogica_036_117-128.pdf  |z Dokumentum-elérés