Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Lezhava, Zaza"'
Autor:
Lezhava, Zaza1, Asanidze, Lasha1, Tsikarishvili, Kukuri1, Karalashvili, Tamaz1, Tolordava, Tamar1
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM. 2023, Vol. 23, p165-172. 8p.
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM. 2021, Vol. 21, p3-10. 8p.
Autor:
Asanidze, Lasha1, Lezhava, Zaza1, Tsikarishvili, Kukuri1, Gaprindashvili, George1,2, Chikhradze, Nino3
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM. 2021, Vol. 21, p59-64. 6p.
Autor:
Lezhava, Zaza1, Asanidze, Lasha1, Tsikarishvili, Kukuri1, Gaprindashvili, George2, Chikhradze, Nino3
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM. 2019, Vol. 19 Issue 1, p3-10. 8p.
Autor:
Asanidze, Lasha1 (AUTHOR) lasha.asanidze@tsu.ge, Lezhava, Zaza1 (AUTHOR), Tsikarishvili, Kukuri1 (AUTHOR), Gaprindashvili, George1,2 (AUTHOR), Chikhradze, Nino3 (AUTHOR), Polk, Jason4 (AUTHOR)
Publikováno v:
Carbonates & Evaporites. Dec2019, Vol. 34 Issue 4, p1205-1212. 8p.
Autor:
Lezhava Zaza, Chartolani Giorgi, Chikhradze Nino, Khomasuridze Zurab, Dvalashvili Giorgi, Bolashvili Nana, Tsikarishvili Kukuri, Dzagnidze Suliko, Naskidashvili Akaki
Publikováno v:
Open Journal of Geology. :1774-1785
Based on the present simultaneous hydrometeorological data and the analysis of the actual materials obtained by our studies, we can suppose the fact of the occurrence of powerful underground floodings in the hydrodynamic system of the Tskaltubo Cave.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28de51ac983f34abb4f1cc791f08b440
https://doi.org/10.4236/ojg.2017.712119
https://doi.org/10.4236/ojg.2017.712119
Autor:
Bolashvili Nana, Lezhava Zaza, Chikhradze Nino, Asanidze Lasha, Chartolani Giorgi, Tsikarishvili Kukuri
Publikováno v:
Earth Sciences. 4:108
One of the important factors of karsto- and speleogenezis of Sataplia-Tskaltubo limestone massif is a still poorly studied geomorphological peculiarity of the region. Karsto- and speleogenezis is conditioned by the geological structure and tectonics.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86a8f9c23164dbaf0920ceefa2cfe62e
https://doi.org/10.11648/j.earth.s.2015040501.30
https://doi.org/10.11648/j.earth.s.2015040501.30