Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Geological profile of the Lubuška pit, Northern Velebit, Croatia (CROSBI ID 663731)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija

Kurečić, Tomislav ; Sudar, Vedran ; Brčić, Vlatko Geological profile of the Lubuška pit, Northern Velebit, Croatia // 26th International Karstological School "Classical Karst" - Show caves and science: abstracts & guide book / Prelovšek, Mitja (ur.). Postojna: ZRC Publishing, 2018. str. 76-76

Podaci o odgovornosti

Kurečić, Tomislav ; Sudar, Vedran ; Brčić, Vlatko

engleski

Geological profile of the Lubuška pit, Northern Velebit, Croatia

The Lubuška pit is located in the area of the Strict Reserve “Hajdučki and Rožanski kukovi“ within the borders of the Northern Velebit National Park. Its entrance is situated at 1495 m above sea level. During previous speleological expeditions the pit has been explored to a depth of 508 m. No detailed geological surveys have been carried out so far, except for scattered observations of structural elements at the shallow parts of the pit. The main aim of the recent geological survey during "Lubuška jama 2017" expedition is to construct of a schematic geological profile of the pit. Two lithological units were observed ; the Velebit (Jelar) breccia and well stratified Jurassic carbonate complex represented by various limestone types. Sampling was carried out across the whole profile below the depth of 240 m, which is also the depth of the contact zone between the Velebit breccia above and the underlying well stratified carbonate complex. Rocks and cave sediment samples were collected at 11 locations throughout the profile of the pit at morphologically specific parts, to ascertain the precise depth of sampling. The contact between the breccia and the carbonate complex has not been precisely established, but most likely it is a tectonic contact. In addition to the sampling, preliminary structural measurements were performed. According to petrographic analysis of rock samples the entire carbonate complex below the Velebit breccia chronostratigraphically belongs to the Callovian-Oxfordian. The specimens include carbonate breccia and limestone variants such as bioclastic wackestone to packstone, micrite limestones and dolomitized limestones. Also, two basic types of clastic sediments were observed: a red silty-clay that fills the cracks in the walls of the channels and stream transported sandy-clay silt deposited next to the siphon lake. The construction of the schematic geological profile of the Lubuška pit is a contribution to the understanding of the geological structure of Hajdučki kukovi area and the broader area of Northern Velebit.

Velebit Mt., Lubuška pit, geological profile

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o prilogu

76-76.

2018.

nije evidentirano

objavljeno

978-961-05-0090-2

Podaci o matičnoj publikaciji

26th International Karstological School "Classical Karst" - Show caves and science: abstracts & guide book

Prelovšek, Mitja

Postojna: ZRC Publishing

Podaci o skupu

26th International Karstological School “Classical Karst”: Speleology

poster

18.06.2018-22.06.2018

Postojna, Slovenija

Povezanost rada

Geologija