Original title:
Lower Cretaceous in the Munella Mountains (Mirdita Zone, northeastern Albania)
Authors:
Peza, Luftulla Hasan ; Marku, D. Document type: Papers Conference/Event: International Cretaceous Symposium /6./, Vienna (AT), 2000-08-27 / 2000-09-04
Year:
2002
Language:
eng Abstract:
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.
Keywords:
Barremian-Aptian; berriasian; Valanginian Project no.: CEZ:AV0Z3013912 (CEP) Host item entry: Aspects of Cretaceous Stratigraphy and Palaeobiogeography. Proceedings of the 6th International Cretaceous Symposium Vienna, 2000
Institution: Institute of Geology AS ČR
(web)
Document availability information: Fulltext is available at the institute of the Academy of Sciences. Original record: http://hdl.handle.net/11104/0043241