The age of the so-called "bostonite" rocks of Mórágy Hill, S-Hungary
MAURTTZ and CSAJÁGHY (1952) could not define exactly the data of consolidation and the genetic origins of the rocks found in the Mórágy granite and which was named "bostonite" by them. These questions have not been answered since that. K/Ar isotopic age of these rocks may reflects that the...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1996
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| Sorozat: | Acta mineralogica-petrographica
37 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24840 |
| Tartalmi kivonat: | MAURTTZ and CSAJÁGHY (1952) could not define exactly the data of consolidation and the genetic origins of the rocks found in the Mórágy granite and which was named "bostonite" by them. These questions have not been answered since that. K/Ar isotopic age of these rocks may reflects that the consolidation happened parallely to that of the rocks of the Early Cretaceous alkaline volcanism. |
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| Terjedelem/Fizikai jellemzők: | 161-164 |
| ISSN: | 0365-8066 |