Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Szabolcs Kósik"'
Publikováno v:
Geoconservation Research, Vol 3, Iss 2, Pp 97-127 (2020)
The Manawatu and Wairarapa regions, lower North Island, are an important geological archive for New Zealand but are not among the iconic geotourism attractions of New Zealand. Recently the geoheritage values of the region have been discussed by vario
Externí odkaz:
https://doaj.org/article/ab9b4e4333d94b94baaba87fd19f46b8
Autor:
Szabolcs Kósik, Takeshi Hasegawa, Martin Danišík, Károly Németh, Makoto Okada, Bjarne Friedrichs, Axel K. Schmitt
Publikováno v:
Earth, Planets and Space, Vol 75, Iss 1, Pp 1-14 (2023)
Abstract Accurate dating of young eruptions from explosive volcanoes is essential for forecasting future eruptions and for defining the hazardscape of volcanic fields. However, precise dating of Quaternary eruptions is often challenging due to limite
Externí odkaz:
https://doaj.org/article/8d463fe8bdab4e6997868ca867c9faac
Autor:
Takeshi Hasegawa, Annika Greve, Darren M. Gravley, Chie Kusu, Yasuaki Kaneda, Shohei Shibata, Makoto Okada, Szabolcs Kósik, Nobutatsu Mochizuki, Gillian Turner
Publikováno v:
Earth, Planets and Space, Vol 75, Iss 1, Pp 1-17 (2023)
Abstract We have carried out paleomagnetic analyses of tephras from the Taupō eruption, one of the most violent eruptions on Earth in the past 5000 years. Pyroclastic deposits were collected with 7 cm3 cubes pushed into each unit of the Taupō erupt
Externí odkaz:
https://doaj.org/article/4d06b9ae6a3446b29fbc12206e2205bc
Autor:
Dávid Karátson, Ralf Gertisser, Tamás Telbisz, Viktor Vereb, Xavier Quidelleur, Timothy Druitt, Paraskevi Nomikou, Szabolcs Kósik
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-8 (2018)
Abstract During the Late Bronze Age, the island of Santorini had a semi-closed caldera harbour inherited from the 22 ka Cape Riva Plinian eruption, and a central island referred to as ‘Pre-Kameni’ after the present-day Kameni Islands. Here, the s
Externí odkaz:
https://doaj.org/article/32fd4c708fdc4970930922bf452f8cf6
Autor:
Károly Németh, Szabolcs Kósik
Publikováno v:
Geosciences, Vol 10, Iss 2, p 44 (2020)
Hydrovolcanism is a type of volcanism where magma and water interact either explosively or non-explosively. The less frequently used term, hydromagmatism, includes all the processes responsible for magma and water interaction in a magmatic system. Hy
Externí odkaz:
https://doaj.org/article/1dea16235b2c48c8aa21498818879838
Autor:
Rafael Torres-Orozco, Shane J. Cronin, Natalia Pardo, Szabolcs Kósik, Ingrid Ukstins, Mirja Heinrich, Peter D. Lee
Highlights • Plinian eruptions linked to rheologically different mingling andesite magmas. • Magma decompression regimes producing variable degassing/crystallization kinetics. • Least explosive eruptions at slowest decompression, ascent and str
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::03413625614fda3d501496f4aa7f3104
http://hdl.handle.net/10044/1/103915
http://hdl.handle.net/10044/1/103915
Publikováno v:
Geological Society, London, Special Publications. 530
Tūhua/Mayor Island is located approximately 45 km off the NE coast of the North Island of New Zealand. This island was formed by various explosive and effusive volcanic eruptions commonly influenced by magma–water interaction eruption events occu
The role of hydrovolcanism in the formation of the Cenozoic monogenetic volcanic fields of Zealandia
Autor:
Károly Németh, Szabolcs Kósik
Publikováno v:
New Zealand Journal of Geology and Geophysics. 63:402-427
Cenozoic geological evolution of New Zealand centres around the formation of Zealandia, a new continent that became detached from the eastern margin of Gondwana around 105 Ma. Spreading opened the ...
Publikováno v:
Geomorphology. 418:108481