Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Duje KUKOČ"'
Autor:
Matija Vukovski, Marko Špelić, Duje Kukoč, Tamara Troskot-Čorbić, Tonći Grgasović, Damir Slovenec, Bruno Tomljenović
Publikováno v:
Swiss Journal of Geosciences, Vol 117, Iss 1, Pp 1-28 (2024)
Abstract A comprehensive study, including geological mapping, structural and thermochronological analysis, has been carried out on Ivanščica Mountain (NW Croatia), with the aim to reconstruct the tectonic history of the Dinarides, Southern/Eastern
Externí odkaz:
https://doaj.org/article/3793d894b134413f9a02f9be225fc8ae
Autor:
Duje Smirčić, Matija Vukovski, Damir Slovenec, Duje Kukoč, Branimir Šegvić, Marija Horvat, Mirko Belak, Tonći Grgasović, Luka Badurina
Publikováno v:
Swiss Journal of Geosciences, Vol 117, Iss 1, Pp 1-24 (2024)
Abstract During the Middle Triassic, intensive volcanic activity took place along the eastern margin of Pangea, including the Greater Adria promontory, due to the Neotethyan oceanization. This resulted in the formation of various volcanic and volcani
Externí odkaz:
https://doaj.org/article/3440aa7d833f4fd0b58faeea135c173e
Autor:
Vlatko Brčić, István Dunkl, Andrea Mindszenty, Mihovil Brlek, Nina Trinajstić, Petra Bajo, Blanca Bauluz, Ivan Mišur, Volker Karius, Sanja Šuica, Duje Kukoč, Alfonso Yuste, Elisa Laita, Hilmar Von Eynatten, Armin Zeh
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Karst bauxite deposits in the North Dalmatian piggyback basin (NDPGB) are a part of the Mediterranean bauxite belt, which is the largest European bauxite deposit zone; however, there is a general lack of information regarding the genesis, age, and pr
Externí odkaz:
https://doaj.org/article/b545d43668f646049d9f7342468f9baa
Publikováno v:
Geologija, Vol 64, Iss 2, Pp 173-188 (2021)
The uppermost Ladinian to Lower Jurassic Zatrnik Formation is the lithostratigraphic unit of the Mesozoic deeper marine Bled Basin. The uppermost part of the Zatrnik Formation and the transition into the overlying Ribnica Breccia was logged at the Za
Externí odkaz:
https://doaj.org/article/b5e601dcb8af4f20b93ea3593f8020a6
Autor:
Mihovil Brlek, Simon Richard Tapster, Julie Schindlbeck-Belo, Sean P. Gaynor, Steffen Kutterolf, Folkmar Hauff, Svetoslav V. Georgiev, Nina Trinajstić, Sanja Šuica, Vlatko Brčić, Kuo-Lung Wang, Hao-Yang Lee, Christoph Beier, Adam B. Abersteiner, Ivan Mišur, Irena Peytcheva, Duje Kukoč, Bianka Németh, Mirka Trajanova, Dražen Balen, Marcel Guillong, Dawid Szymanowski, Réka Lukács
Publikováno v:
Gondwana Research. 116:40-60
The Carpathian-Pannonian Region (CPR) hosted some of the largest silicic volcanic eruptions in Europe during the Early and Middle Miocene, contemporaneously with major lithospheric thinning of the Pannonian Basin. This was recorded as an ignimbrite f
Autor:
Duje Kukoč, Duje Smirčić, Tonći Grgasović, Marija Horvat, Mirko Belak, Dražen Japundžić, Tea Kolar-Jurkovšek, Branimir Šegvić, Luka Badurina, Matija Vukovski, Damir Slovenec
Publikováno v:
International Journal of Earth Sciences. 112:1175-1201
Publikováno v:
Folia biologica et geologica. 63:61-83
The Julian Alps belong to the eastern Southern Alps where the South-Alpine and the Dinaric structures now overlap. In Mesozoic times, this area was part of the northeastern Adriatic continental margin, which was facing the Neotethys Ocean but was als
Autor:
Špela Goričan, Martin Đaković, Peter O. Baumgartner, Hans-Jürgen Gawlick, Tim Cifer, Nevenka Djerić, Aleksander Horvat, Anja Kocjančič, Duje Kukoč, Milica Mrdak
Publikováno v:
Folia biologica et geologica. 63:85-150
The Dinarides, together with the Albanides and Hellenides, preserve stratigraphic successions derived from the eastern margin of the Adriatic microplate and remnants of ophiolites obducted from the Maliac-Vardar branch of the Neotethys Ocean. The mai
Publikováno v:
Geologija, Vol 64, Iss 2, Pp 173-188 (2021)
Geologija, vol. 64, no. 2, pp. 173-188, 2021.
Geologija, vol. 64, no. 2, pp. 173-188, 2021.
The uppermost Ladinian to Lower Jurassic Zatrnik Formation is the lithostratigraphic unit of the Mesozoic deeper marine Bled Basin. The uppermost part of the Zatrnik Formation and the transition into the overlying Ribnica Breccia was logged at the Za
Ivanščica Mt. is an inselberg in the transitional area where S-verging Southern Alpine structures overprint NNW-verging Dinaric structures (van Gelder et al. 2015, and references therein). It is composed of Triassic to Cretaceous shallow to deep-ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4af6842d52e4674098e663210455de3
https://doi.org/10.5194/egusphere-alpshop2022-23
https://doi.org/10.5194/egusphere-alpshop2022-23