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 !

Geologija Papuka (CROSBI ID 54686)

Prilog u knjizi | izvorni znanstveni rad

Balen, Dražen Geologija Papuka // 5. hrvatski geološki kongres s međunarodnim sudjelovanjem - Vodič ekskurzija / Horvat, Marija ; Galović, Lidija (ur.). Zagreb: Hrvatski geološki institut, 2015. str. 3-90

Podaci o odgovornosti

Balen, Dražen

hrvatski

Geologija Papuka

Following the excursion “A0 Geological heritage of the Papuk Geopark” related to the 4th Croatian Geological Congress in 2010, this excursion is planned as a complementary one with emphasizes on geological diversity of Mt. Papuk and neighboring areas which are accessible to a larger group of geologist transported by bus. The excursion points to the main features of Mt. Papuk (and Mt. Krndija) crystalline rocks, Paleozoic and Mesozoic (meta)sedimentary complexes together with sedimentary and volcanic rocks of Pannonian Basin with highlights on evolution(s) of broader area through time, origin of rocks, emplacement, conditions, petrography, paleontological findings and ages. In the Slavonia area, the pre-Mesozoic crystalline basement of the Pannonian Basin, which represents the highlight of the field-trip, is traditionally subdivided into three igneous and metamorphic complexes (eg. JAMIČIĆ, 1988): (1) the Psunj (Kutjevo) complex, assumed to have originated during the Late Precambrian to Early Paleozoic time span, overprinted and retrogressed by younger metamorphic events ; (2) the Papuk (Jankovac) complex, which underwent significant geological changes during the Ordovician to Early Devonian period, and (3) the Radlovac complex which presumably resulted from a very low- to low-grade metamorphism during the Late Paleozoic. Overlying Permian-Triassic rocks are coarse- to medium- grained terrigeneous clastics, i.e. conglomerates and sandstones that are in unconformable contact with metamorphic complexes and grade into Lower Triassic sandstones. Composition of detrital components indicates magmatic and metamorphic rocks of the surrounding area as an adjacent source region. The clastic rocks crop out as elongated narrow zones, occurring between the crystalline complexes and the Middle Triassic, predominately carbonate rocks. Thermal overprint that took place during Eoalpine (Cretaceous) time affected predominately clay minerals, thus leaving hardly noticeable marks and reassigning (in the strict sense of metamorphic classification) the Mesozoic sedimentary rock complex into the very-low grade metasediments. Sedimentation in Oligocene and further during Neogene is related to the closing of Tethys, evolution of Central Paratethys and finally to development of new separate area which encompasses Pannonian Basin System. This area is a more or less isolated area starting from Oligocene time developing its own sedimentation characteristics accompanied with volcanic activities. Past volcanic activity produced a heterogeneous and quite large volcanic complex famous due to extraordinary, well-exposed columnar jointing and pyroclastic rock deposits. Recent sedimentation is represented with a tufa barrier at the Skakavac waterfall in the vicinity of the Jankovac mountain hut. The chosen outcrops comprise selection of typical rocks at localities Puklica, Rupnica, Trešnjevica, Zvečevo, Čarugin kamen, Vranovo, Šamanovica, Nježić, Velika, Jankovac, Hercegovac, Žervanjska, Tisica, Vetovo, Kutjevo, Duboka, Lončarski Vis and Našice revealing geological relations important for setting the area in geological and geotectonic frame(s) through Paleozoic, Mesozoic and Cenozoic times. Geological field-trip in such an area would not be complete without Golden Valley’s wines, cultivated in ancient wine-cellars, first built by the clerical order of Cistercians (ordo cisterciensis) in 1232. The modern vineyards have been spread on the southern slopes of the mountains Papuk and Krndija in a constant and devoted search for the perfect harmony between the climate, sun, soil and rocks. Kutjevo wine-cellars with skilled cellarers achieve the top-level quality of wines. Some of the famous wines from the Kutjevo area are: Graševina, Rheinriesling, Chardonnay, Pinot Gris, Pinot Noir, Pinot Blanc, Sauvignon, Traminac.

Papuk, geologija

Dio točaka opisanih u vodiču istraživan je u sklopu projekta HRZZ IP-2014-09-9541.

engleski

Geology of Mt. Papuk

nije evidentirano

Mt Papuk, geology

nije evidentirano

Podaci o prilogu

3-90.

objavljeno

Podaci o knjizi

5. hrvatski geološki kongres s međunarodnim sudjelovanjem - Vodič ekskurzija

Horvat, Marija ; Galović, Lidija

Zagreb: Hrvatski geološki institut

2015.

978-953-6907-50-1

Povezanost rada

Povezane osobe




nije evidentirano