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pro vyhledávání: '"Kalvoda, Jirí"'
Given a graph $G$, we say that an orientation $D$ of $G$ is a KT orientation if, for all $u, v \in V(D)$, there is at most one directed path (in any direction) between $u$ and $v$. Graphs that admit such orientations have been used by Kierstead and T
Externí odkaz:
http://arxiv.org/abs/2407.18346
Autor:
Vodrážková, Stanislava, Kumpan, Tomáš, Vodrážka, Radek, Frýda, Jiří, Čopjaková, Renata, Koubová, Magdalena, Munnecke, Axel, Kalvoda, Jiří, Holá, Markéta
Publikováno v:
In Sedimentary Geology August 2022 438
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In Sedimentary Geology June 2020 402
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 October 2019 531 Part A
Publikováno v:
In Sedimentary Geology February 2019 380:143-157
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 15 March 2018 493:30-43
Autor:
Bábek, Ondřej, Faměra, Martin, Šimíček, Daniel, Weinerová, Hedvika, Hladil, Jindřich, Kalvoda, Jiří
Publikováno v:
In Global and Planetary Change January 2018 160:75-95
Publikováno v:
In Geobios August 2017 50(4):341-348
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In Geobios September-October 2016 49(5):349-354
Publikováno v:
In Sedimentary Geology 15 May 2016 337:81-99