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Upper Cretaceous-Palaeogene Tholeiitic Basalts of the Southern Margin of the Pannonian Basin: Pozeska gora Mt. (Croatia)

M. Belak
J. Halamić
V. Marchig
D. Tibljaš


Puni tekst: engleski pdf 6.915 Kb

str. 163-174

preuzimanja: 586

citiraj


Sažetak

According to the geological relationships in the region of Pozeska gora Mt. (the southern margin of the Pannonian Basin, northern Croatia), basic eruptive rocks are considered to be of Upper Cretaceous-Palaeogene age. Detailed petrographic examination, based on physiographic description, the chemical composition of major and trace elements, rare earth elements and stable isotopes, indicates that these primary tholeiitic basalts have variable structural-textural characteristics, and were postmagmatically affected by metamorphic processes. Tholeiitic basalts originated from the upper mantle, and were placed in the form of subaquatic effusions in the extensional zones within continental crust.

Ključne riječi

Tholeiitic basalts; Upper Cretaceous-Palaeogene; Upper mantle; Pannonian Basin; Pozeska gora Mt.; Croatia

Hrčak ID:

3903

URI

https://hrcak.srce.hr/3903

Datum izdavanja:

30.12.1998.

Posjeta: 1.338 *