THE SULOV PALEOGENE OF THE DOMANIZA BASIN IN THE LIGHT OF NEW FINDINGS

In: Geologica Carpathica, vol. 44, no. 2

Jozef Salaj

Detaily:

Rok, strany: 1993, 95 - 104

O článku:

The newly defined Svinske Chlievy Formation in the Pruzina part of the Domaniza Basin, is equivalent in age to the laterally represented Sulov Formation. It corresponds to the uppermost Paleocene (base of the Ilerdian) and the greater part of the Lower Eocene. It is a complex of rocks, which, apart from transgressive marine basins, originated in continental conditions of sedimentation.

Ako citovať:

ISO 690:

Salaj, J. 1993. THE SULOV PALEOGENE OF THE DOMANIZA BASIN IN THE LIGHT OF NEW FINDINGS. In Geologica Carpathica, vol. 44, no.2, pp. 95-104. 1335-0552.

APA:

Salaj, J. (1993). THE SULOV PALEOGENE OF THE DOMANIZA BASIN IN THE LIGHT OF NEW FINDINGS. Geologica Carpathica, 44(2), 95-104. 1335-0552.