During the Variscan orogenic cycle, central Europe was intruded by numerous granitoid plutons. Typological and age relationships show that the characteristics of the granitoid magmatism changed during the course of the Variscan orogeny. Five genetic groups of granitoids may be distinguished (partial abstract)
|Number of pages||29|
|Journal||Mineralogy and Petrology|
|Publication status||Published - 1997|
Finger, F., Roberts, M., Haunschmid, B., Schermaier, A., & Steyrer, H-P. (1997). Variscan granitoids of central Europe: their typology, potential sources and tectonothermal relations. Mineralogy and Petrology, 61, 67-96.