Structural evolution of the Peninsular Gneiss — an early Precambrian migmatitic complex from South India

@article{Naha1990StructuralEO,
  title={Structural evolution of the Peninsular Gneiss — an early Precambrian migmatitic complex from South India},
  author={Kshitindramohan Naha and Raghavan Srinivasan and S. Jayaram},
  journal={Geologische Rundschau},
  year={1990},
  volume={79},
  pages={99-109}
}
ZusammenfassungDer Peninsula-Gneis, der von einigen Bearbeitern als das Basement angesehen wird, auf dem die Gesteine der Dharwar-Gruppe abgelagert wurden, ist ein Migmatit aus Komponenten älterer metamorpher Sedimentgesteine und Magmatite. Abfolge der Deformation und Deformationsart dieser Gneise entspricht der Deformation des Dharwar Schiefergürtels. Die Hauptmigmatisierung verlief zeitgleich mit der isoklinalen ersten Faltung, die von einer zweiten fast coaxialen und einer dritten aufrecht… 
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