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pro vyhledávání: '"KLIMCHOUK, Alexander"'
Autor:
Klimchouk, Alexander, Evans, David, Milanovic, Sasa, Bittencourt, Cristian, Sanchez, Mauro, Carlos Aguirre, F.
Publikováno v:
In Geomorphology 1 January 2023 420
Autor:
Dublyansky, Yuri V., Klimchouk, Alexander B., Tokarev, Sergey V., Amelichev, Gennady N., Langhamer, Lukas, Spötl, Christoph
Publikováno v:
In Journal of Hydrology October 2018 565:61-73
Autor:
Klimchouk, Alexander, Auler, Augusto S., Bezerra, Francisco H.R., Cazarin, Caroline L., Balsamo, Fabrizio, Dublyansky, Yuri
Publikováno v:
In Geomorphology 15 January 2016 253:385-405
Autor:
Ennes-Silva, Renata A., Bezerra, Francisco H.R., Nogueira, Francisco C.C., Balsamo, Fabrizio, Klimchouk, Alexander, Cazarin, Caroline L., Auler, Augusto S.
Publikováno v:
In Tectonophysics 15 January 2016 666:244-259
Akademický článek
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Publikováno v:
International Journal of Speleology, Vol 41, Iss 2, Pp 161-179 (2012)
In carbonate rocks, especially in those with high primary porosity such as most Cenozoic carbonates, the interaction between deeply derived rising flow through sub-vertical fracture-controlled conduits and intrastratal matrix flow of shallower system
Externí odkaz:
https://doaj.org/article/d807771650724faa9d654eaeaa753da7
Autor:
Klimchouk Alexander
Publikováno v:
International Journal of Speleology, Vol 35, Iss 1, Pp 19-24 (2006)
Speleogenesis in confined settings generates cave morphologies that differ much from those formed in unconfined settings. Cavesdeveloped in unconfined settings are characterised by broadly dendritic patterns of channels due to highly competing develo
Externí odkaz:
https://doaj.org/article/a1776e15fb3d4cb880bdfeced1c39301
Autor:
Klimchouk Alexander
Publikováno v:
International Journal of Speleology, Vol 34, Iss 1-2, Pp 45-64 (2005)
Conceptual and respective quantitative models of speleogenesis/karstifi cation developed for unconfi ned aquifers do not adequately representspeleogenesis in confi ned settings. A conceptual model for speleogenesis in confi ned settings is suggested,
Externí odkaz:
https://doaj.org/article/0bb4065cfa3d433c84fb055131b82279
Publikováno v:
International Journal of Speleology, Vol 31, Iss 1-4, Pp 55-88 (2002)
The term karst breakdown is employed in this paper to denote the totality of processes and phenomena of gravitational and/or hydrodynamic destruction of the ceiling of a karst cavity and of the overlying sediments. It refers not only to the existence
Externí odkaz:
https://doaj.org/article/4e7b993497a34c5096f5889cfd1fcb58