Facebook Instagram Twitter RSS Feed PodBean Back to top on side

Isopodichnus AND OTHER TRACE FOSSILS FROM MARINE KOPIENIEC FORMATION (RHAETIAN-SINEMURIAN) IN THE TATRA MTS., POLAND

In: Geologica Carpathica, vol. 42, no. 2
Alfred Uchman
Detaily:
Rok, strany: 1991, 117 - 121
Jazyk: eng
O článku:
Trace fossils: Planolites, Palaeophycus, Chondrites, Asteriacites, Thalassinoides and Isopodichnus, occur in the marine fauna of fossiliferous Kopieniec Formation of the Krizna Nappe in the Polish Tatra Mts. The latter is described mainly in non-marine. deposits. This assemblage resembles the Cruziana ichnofacies.
Ako citovať:
ISO 690:
Uchman, A. 1991. Isopodichnus AND OTHER TRACE FOSSILS FROM MARINE KOPIENIEC FORMATION (RHAETIAN-SINEMURIAN) IN THE TATRA MTS., POLAND. In Geologica Carpathica, vol. 42, no.2, pp. 117-121. 1335-0552.

APA:
Uchman, A. (1991). Isopodichnus AND OTHER TRACE FOSSILS FROM MARINE KOPIENIEC FORMATION (RHAETIAN-SINEMURIAN) IN THE TATRA MTS., POLAND. Geologica Carpathica, 42(2), 117-121. 1335-0552.