Lower Cretaceous in the Munella Mountains (Mirdita Zone, northeastern Albania)

0145675 - GLU-S 20033046 RIV CZ eng C - Konferenční příspěvek (zahraniční konf.)
Peza, Luftulla Hasan - Marku, D.
Lower Cretaceous in the Munella Mountains (Mirdita Zone, northeastern Albania).
3-7001-3089-9. In: Aspects of Cretaceous Stratigraphy and Palaeobiogeography. Proceedings of the 6th International Cretaceous Symposium Vienna, 2000. Wien: Österreichische Akademie der Wissenschaften Schriftenreihe der Erdwissenschaftlichen Kommissionen., 2002 - (Wagreich, M.), s. 365-372. Österreichische Akademie der Wissenschaften Schriftenreihe der Erdwissenschaftlichen Kommissionen.
[International Cretaceous Symposium /6./. Vienna (AT), 27.08.2000-04.09.2000]
Výzkumný záměr: CEZ:AV0Z3013912
Klíčová slova: berriasian * Valanginian * Barremian-Aptian
Kód oboru RIV: DB - Geologie a mineralogie

The Munella Mountain is located in the Mirdita area, in the northeastern part of Albania. Berrisian, Valanginian deep-water flysch deposits. Unsorted breccias, including large blocks of ophiolites and Triassic limestones lie at the base of the Berriasian. Marls, sandstones, conglomerates with rare limestone intercalations characterize the upper part of the Berriasian. Sandstones and marls with abundant molluscs form the base of the Barremian-Aptian deposits. The highhest part of the section consists of platform limestones in Urgonian facies. An interruption in sedimentation during the Hauterivian was caused by the Mirditean orogeny.
Trvalý link: http://hdl.handle.net/11104/0043241