Analogie budowy geologicznej waryscydów antyklinorium śląsko-krakowskiego z Sudetami i Górami Świętokrzyskimi
Abstract
ANALOGY IN GEOLOGICAL STRUCTURE OF VARISCIDES OF THE SILESIAN-MORAVIAN ANTICLINORIUM WITH SUDETES AND HOLY CROSS MTS
Summary
The Upper Silesian Coal Basin formed on the Cieszyn block is embraced by two Variscian branches. The Silesian-Moravian Variscides were formed due to eugeosynclinal development, the Cracow Variscides, however, due to miogeosynclinal one. The Variscides show a great analogy in diastrophic-sedimentary and magmatic development with the Variscides of the Holy Cross Mts.
Summary
The Upper Silesian Coal Basin formed on the Cieszyn block is embraced by two Variscian branches. The Silesian-Moravian Variscides were formed due to eugeosynclinal development, the Cracow Variscides, however, due to miogeosynclinal one. The Variscides show a great analogy in diastrophic-sedimentary and magmatic development with the Variscides of the Holy Cross Mts.