TECTONICS OF THE HORNONITRIANSKA KOTLINA DEPRESSION IN THE NEOGENE

In: Geologica Carpathica, vol. 46, no. 4

Jozef Hok - Ladislav Simon - Peter Kovac - Michal Elecko - Dionyz Vass - Jozef Halmo - Frantisek Verbich

Detaily:

Rok, strany: 1995, 191 - 196

Jazyk: eng

O článku:

Brittle deformation analysis of the Tertiary depression fill and surrounding area of the Hornonitrianska Kotlina Depression permited the reconstruction of the paleostress-field orientation. Compression axis rotated clockwise from NW-SE (Early Miocene) to NE-SW (Middle Miocene). After Middle Miocene (Middle Sarmatian) compression axis rotated counterclockwise to the NNW-SSE position in Quaternary. During the Early Miocene the marine sedimentation predominated. The marine conditions appeared again during Early Badenian, but later continental conditions prevailed.

Ako citovať:

ISO 690:

Hok, J., Simon, L., Kovac, P., Elecko, M., Vass, D., Halmo, J., Verbich, F. 1995. TECTONICS OF THE HORNONITRIANSKA KOTLINA DEPRESSION IN THE NEOGENE. In Geologica Carpathica, vol. 46, no.4, pp. 191-196. 1335-0552.

APA:

Hok, J., Simon, L., Kovac, P., Elecko, M., Vass, D., Halmo, J., Verbich, F. (1995). TECTONICS OF THE HORNONITRIANSKA KOTLINA DEPRESSION IN THE NEOGENE. Geologica Carpathica, 46(4), 191-196. 1335-0552.