Age, geochemistry and origin of peraluminous A-type granitoids of the Ablah-Shuwas pluton, Ablah graben, Arabian Shield
The A-type granitoids of the Ablah-Shuwas pluton, situated in the Ablah graben of the Asir terrane, occur as discontinuous ring complexes, cone sheets and irregular bodies. They intrude into the younger diorite and tonalite rocks of probably 744±22 Ma old. Their emplacement is contemporaneous with t...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
Department of Mineralogy, Geochemistry and Petrology, University of Szeged
Szeged
2001
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| Sorozat: | Acta mineralogica-petrographica
42 |
| Kulcsszavak: | Földtan, Kőzettan, Ásványtan, Geokémia |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/25085 |