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THE CENTRAL SLOVAK FAULT SYSTEM — THE FIELD EVIDENCE OF A STRIKE SLIP

In: Geologica Carpathica, vol. 44, no. 3
Peter Kovac - Jozef Hok

Details:

Year, pages: 1993, 155 - 159
About article:
The main aim of this paper is to understand the tectonic activity of the Central Slovak Fault System during Late Eocene to Miocene period. During this time the strike-slip faults influenced the structure of the Western Carpathians. Both regional fault patterns and their kinematics are a result of the regional stress field. The fault analysis along the Central Slovak Fault System enables to reconstruct the distribution of paleostresses. NE-SW (Late? Paleocene–Middle Miocene) as well as NW-SE distensions (Middle–Late Miocene) have been identified.
How to cite:
ISO 690:
Kovac, P., Hok, J. 1993. THE CENTRAL SLOVAK FAULT SYSTEM — THE FIELD EVIDENCE OF A STRIKE SLIP. In Geologica Carpathica, vol. 44, no.3, pp. 155-159. 1335-0552.

APA:
Kovac, P., Hok, J. (1993). THE CENTRAL SLOVAK FAULT SYSTEM — THE FIELD EVIDENCE OF A STRIKE SLIP. Geologica Carpathica, 44(3), 155-159. 1335-0552.