@article{MTMT:34429588,
	title = {Boulder distribution, circular polarization, and optical maturity: A survey of example lunar polar terrains for future landing sites},
	url = {https://m2.mtmt.hu/api/publication/34429588},
	author = {Tomka, Richárd Krisztián and Boazman, S. and Bradák, B. and Heather, D.J. and Kereszturi, A. and Pal, B.D. and Steinmann, Vilmos},
	doi = {10.1016/j.asr.2023.10.005},
	journal-iso = {ADV SPACE RES},
	journal = {ADVANCES IN SPACE RESEARCH},
	volume = {73},
	unique-id = {34429588},
	issn = {0273-1177},
	year = {2024},
	eissn = {1879-1948},
	pages = {2243-2260},
	orcid-numbers = {Pal, B.D./0000-0002-7189-1627; Steinmann, Vilmos/0000-0001-5233-6436}
}

@article{MTMT:34471880,
	title = {Morphological analysis of polar landing regions for a solar powered ice drilling mission},
	url = {https://m2.mtmt.hu/api/publication/34471880},
	author = {Tomka, Richárd Krisztián and Steinmann, Vilmos and Warren, T. and Kereszturi, A.},
	doi = {10.1016/j.icarus.2023.115927},
	journal-iso = {ICARUS},
	journal = {ICARUS},
	volume = {411},
	unique-id = {34471880},
	issn = {0019-1035},
	year = {2023},
	eissn = {1090-2643},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@article{MTMT:33110824,
	title = {Characteristics of de Gerlache crater, site of girlands and slope exposed ice in a lunar polar depression},
	url = {https://m2.mtmt.hu/api/publication/33110824},
	author = {Kereszturi, Ákos and Tomka, Richárd Krisztián and Gläser, P. A. and Pál, Bernadett and Steinmann, Vilmos and Warren, T.},
	doi = {10.1016/j.icarus.2022.115231},
	journal-iso = {ICARUS},
	journal = {ICARUS},
	volume = {388},
	unique-id = {33110824},
	issn = {0019-1035},
	abstract = {The 31 km diameter and 7.5 km deep de Gerlache crater, located 30 km from the southern pole of the Moon was surveyed. At its bottom a 15 km diameter younger crater can be also found beside many smaller overprinting craters. At moderately sloping terrains a few m high, 100-200 m wide, curving quasi-parallel, km long set of ridges could be identified, which seem to be widespread on the surface, and might cover the half or even more of the crater. We named these "girland like features" in this work, which seem to be produced by mass movements on slopes (however differ from most of the already identified slope features, which show downslope elongated lineaments or fallen/redeposited debris on the Moon). At all locations they are superposed by recently formed 10-50 m diameter craters, thus might be older than the equilibrium crater population shown age of about 100 Ma old. This is the first identification of these features at the polar terrains, where they might contribute both in the shielding or exposing of subsurface ice. In de Gerlache crater ice occurrences have previously been located on moderately steep slopes, indicating they might be exposed by mass movement processes, where active movements might have happened in the last some 10 Ma using crater statistics based age of the shallow regolith layer. Only half of them were located at areas with modelled surface temperatures below 110 K, where temperature might be not enough to keep most of the deposited H2O there on Ga time scale. However the real values are probably more diverse because of the limited spatial resolution of available temperature data. Target areas are indicated for possible future missions, where periodic solar illumination, and subsurface ice at 0.5 m depth could be also present.},
	keywords = {Moon; POLAR ICE; DeGerlache crater},
	year = {2022},
	eissn = {1090-2643},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@CONFERENCE{MTMT:33100223,
	title = {Marsi és mars-analóg földi folyóvölgyek fluviális összehasonlítása kvantitatív adatok alapján},
	url = {https://m2.mtmt.hu/api/publication/33100223},
	author = {Steinmann, Vilmos},
	booktitle = {Intézményi ÚNKP Konferencia 2022},
	unique-id = {33100223},
	year = {2022},
	pages = {193},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@article{MTMT:33044679,
	title = {The magnetic susceptibility of Pleistocene paleosols as a Martian paleoenvironment analog},
	url = {https://m2.mtmt.hu/api/publication/33044679},
	author = {Bradák, Balázs and Kereszturi, Ákos and Steinmann, Vilmos and Gomez, C and Csonka, Diána and Hyodo, M and Szeberényi, József and Novothny, Ágnes and Végh, Tamás and Barta, Gabriella and Medveďová, A and Rostinsky, P and Mihály, Enikő and Jó, Viviána and Horváth, Erzsébet},
	doi = {10.1016/j.icarus.2022.115210},
	journal-iso = {ICARUS},
	journal = {ICARUS},
	volume = {387},
	unique-id = {33044679},
	issn = {0019-1035},
	year = {2022},
	eissn = {1090-2643},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436; Csonka, Diána/0000-0002-2318-6720; Novothny, Ágnes/0000-0003-3513-0406; Végh, Tamás/0000-0001-8476-3686; Barta, Gabriella/0000-0002-5460-1085; Horváth, Erzsébet/0000-0002-0197-4152}
}

@article{MTMT:32601520,
	title = {Testing statistical impact crater analysis in permanently shadowed lunar polar regions},
	url = {https://m2.mtmt.hu/api/publication/32601520},
	author = {Kereszturi, Ákos and Tomka, Richárd Krisztián and Steinmann, Vilmos},
	doi = {10.1016/j.icarus.2022.114879},
	journal-iso = {ICARUS},
	journal = {ICARUS},
	volume = {376},
	unique-id = {32601520},
	issn = {0019-1035},
	year = {2022},
	eissn = {1090-2643},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@article{MTMT:32619025,
	title = {Formation timescale model for a small sized Martian fluvial valley},
	url = {https://m2.mtmt.hu/api/publication/32619025},
	author = {Steinmann, Vilmos and Kereszturi, Ákos},
	doi = {10.5194/epsc2021-212},
	journal-iso = {EPSC ABSTRACTS},
	journal = {EPSC ABSTRACTS},
	volume = {15},
	unique-id = {32619025},
	year = {2021},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@{MTMT:32006541,
	title = {Geomorphological Analysis and Erosion Modelling of a Martian Fluvial System},
	url = {https://m2.mtmt.hu/api/publication/32006541},
	author = {Steinmann, Vilmos},
	booktitle = {Recent Developments in Geomorphology Research},
	unique-id = {32006541},
	year = {2021},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@inproceedings{MTMT:32072796,
	title = {A hidroszféra felszíni lefolyásnyomai - folyóvölgyek a Marson},
	url = {https://m2.mtmt.hu/api/publication/32072796},
	author = {Steinmann, Vilmos},
	booktitle = {Hidroszféra: a víz mint különleges anyag : a hidroszféra a Földön és a Naprendszer más égitestjein},
	doi = {10.31852/EMF.32.2020.073.080},
	unique-id = {32072796},
	year = {2020},
	pages = {73-80},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436}
}

@article{MTMT:31787492,
	title = {Geomorphological analysis of Tinto-B Vallis on Mars},
	url = {https://m2.mtmt.hu/api/publication/31787492},
	author = {Steinmann, Vilmos and Kereszturi, Ákos and Mari, László},
	doi = {10.15201/hungeobull.69.4.1},
	journal-iso = {HUNG GEOGR BULL (2009-)},
	journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)},
	volume = {69},
	unique-id = {31787492},
	issn = {2064-5031},
	year = {2020},
	eissn = {2064-5147},
	pages = {333-348},
	orcid-numbers = {Steinmann, Vilmos/0000-0001-5233-6436; Kereszturi, Ákos/0000-0001-6420-510X; Mari, László/0000-0002-3382-7800}
}