@article{MTMT:34611738,
	title = {Archeoseismic Study of Damage in Medieval Monuments around New Delhi, India: An Approach to Understanding Paleoseismicity in an Intraplate Region},
	url = {https://m2.mtmt.hu/api/publication/34611738},
	author = {Naik, Sambit Prasanajit and Reicherter, Klaus and Kázmér, Miklós and Skapski, Jens and Mohanty, Asmita and Kim, Young-Seog},
	doi = {10.3390/geohazards5010007},
	journal-iso = {GeoHazards},
	journal = {GeoHazards},
	volume = {5},
	unique-id = {34611738},
	abstract = {The seismic shaking observed around Delhi and the surrounding region due to near-field and far-field earthquakes is a matter of concern for the seismic safety of the national capital of India, as well as the historical monuments of the region. Historical seismicity indicates that the Delhi region has been affected by several damaging earthquakes originating from the Himalayan region as far-field events, as well as due to near-field earthquakes with epicenters close to Delhi. The historical records, along with recent archeoseismological studies, suggest that Qutab Minar, a UNESCO World Heritage Site, was damaged by the earthquake of 1803 CE. This event represents the only evidence of seismic damage from the region, as there has been no detailed study of other historical monuments in the area or earthquakes that have caused damage. In this context, the earthquake damage to other monuments might have been overlooked to some extent around the Qutab Minar due to the lack of proper earthquake damage surveys and documentation in historical times. The main goal of this study is to identify evidence of earthquake archeological effects around the Qutab Minar and to shed new light on the occurrence and characteristics of ancient earthquakes while providing data to inform seismic risk assessment programs. With this aim, we describe different earthquake-related damage (EAE, earthquake archeological effects) at the Isa Khan Tomb and Humayun’s Tomb, built between 1548 CE and 1570 CE, respectively, as well as the older Tomb of Iltutmish (built in 1235 CE) along with the Qutab Minar, which was built between 1199 CE and 1220 CE. The damage was probably caused by seismic events with intensities between VIII and IX on the European Macroseismic Scale (EMS). Based on the methodology of paleo ShakeMaps, it is most likely that the 1803 CE earthquake was the causative earthquake for the observed deformation in the Isa Khan Tomb, Tomb of Iltutmish, and Humayun’s Tomb. More detailed regional paleoseismological studies are required to identify the responsible fault. In conclusion, the impressive cultural heritage of Delhi city and the intraplate region is constantly under seismic threats from near-field earthquakes and far-field Himalayan earthquakes.},
	year = {2024},
	eissn = {2624-795X},
	pages = {142-165},
	orcid-numbers = {Naik, Sambit Prasanajit/0000-0001-7324-8291; Reicherter, Klaus/0000-0002-9339-4488; Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:34686343,
	title = {Visegrád pusztulása az oszmán-török hódoltság előtt – az 1541-es földrengés történeti és archeoszeizmológiai nézőpontból},
	url = {https://m2.mtmt.hu/api/publication/34686343},
	author = {Kázmér, Miklós and Al-Tawalbeh, Mohammad Ibrahim Abed and Győri, Erzsébet and Laszlovszky, József and Gaidzik, K},
	doi = {10.23928/foldt.kozl.2023.153.4.357},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {153},
	unique-id = {34686343},
	issn = {0015-542X},
	year = {2023},
	eissn = {2559-902X},
	pages = {357-374},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@{MTMT:34611804,
	title = {I. e. 1.500.000 körül - Kiemelkedik a Kárpátok},
	url = {https://m2.mtmt.hu/api/publication/34611804},
	author = {Kázmér, Miklós},
	booktitle = {Magyarország globális története a kezdetektől 1868-ig},
	unique-id = {34611804},
	year = {2023},
	pages = {15-17},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:33892558,
	title = {Seismic catastrophes in historical times in Arabia – Destruction of the city of Qalhat (Oman) in the 16th century},
	url = {https://m2.mtmt.hu/api/publication/33892558},
	author = {Kázmér, Miklós and Gaidzik, Krzysztof and Al-Tawalbeh, Mohammad and Steinritz, Vanessa and Reicherter, Klaus and Hoffmann, Gösta},
	doi = {10.1016/j.quaint.2023.05.016},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {664},
	unique-id = {33892558},
	issn = {1040-6182},
	year = {2023},
	eissn = {1873-4553},
	pages = {42-58},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316; Gaidzik, Krzysztof/0000-0003-3286-0833; Al-Tawalbeh, Mohammad/0000-0003-4917-5795; Steinritz, Vanessa/0000-0001-8483-2434; Reicherter, Klaus/0000-0002-9339-4488; Hoffmann, Gösta/0000-0002-2605-2672}
}

@article{MTMT:33611038,
	title = {Seismic Activity in the Celje Basin (Slovenia) in Roman Times—Archaeoseismological Evidence from Celeia},
	url = {https://m2.mtmt.hu/api/publication/33611038},
	author = {Kázmér, Miklós and Jamšek Rupnik, Petra and Gaidzik, Krzysztof},
	doi = {10.3390/quat6010010},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {6},
	unique-id = {33611038},
	issn = {2571-550X},
	abstract = {Searching for unknown earthquakes in Slovenia in the first millennium, we performed archaeoseismological analysis of Roman settlements. The Mesto pod mestom museum in Celje exhibits a paved Roman road, which suffered severe deformation. Built on fine gravel and sand from the Savinja River, the road displays a bulge and trench, pop-up structures, and pavement slabs tilted up to 40°. The city wall was built over the deformed road in Late Roman times, supported by a foundation containing recycled material (spolia) from public buildings, including an emperor’s statue. We hypothesize that a severe earthquake hit the town before 350 AD, causing widespread destruction. Seismic-induced liquefaction caused differential subsidence, deforming the road. One of the nearby faults from the strike-slip Periadriatic fault system was the seismic source of this event.},
	year = {2023},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316; Jamšek Rupnik, Petra/0000-0003-0809-1739; Gaidzik, Krzysztof/0000-0003-3286-0833}
}

@article{MTMT:33479632,
	title = {The Børglum fault was active in historical times. Comment on ‘The near-surface structure in the area of the Børglum fault, Sorgenfrei-Tornquist Zone, northern Denmark: Implications for fault kinematics, timing of fault activity and fault control on tunnel valley formation’ by Brandes et al. [Quat. Sci. Rev. 289 (2022) 107619]},
	url = {https://m2.mtmt.hu/api/publication/33479632},
	author = {Gaidzik, Krzysztof and Kázmér, Miklós},
	doi = {10.1016/j.quascirev.2022.107933},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {301},
	unique-id = {33479632},
	issn = {0277-3791},
	year = {2023},
	eissn = {1873-457X},
	orcid-numbers = {Gaidzik, Krzysztof/0000-0003-3286-0833; Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:34065081,
	title = {Két földrengés az ókori Palesztinában : Capitolias római színházának archeoszeizmológiája},
	url = {https://m2.mtmt.hu/api/publication/34065081},
	author = {Lakatos, Szilvia and Al-Tawalbeh, Mohammad Ibrahim Abed and Khrisat, Bilal and Kázmér, Miklós},
	journal-iso = {ÓKOR},
	journal = {ÓKOR: FOLYÓIRAT AZ ANTIK KULTÚRÁRÓL},
	volume = {21},
	unique-id = {34065081},
	issn = {1589-2700},
	year = {2022},
	pages = {66-77},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:33542592,
	title = {Banjarmasin: public health and social structure in 1877, as described by a Hungarian medical doctor and geologist},
	url = {https://m2.mtmt.hu/api/publication/33542592},
	author = {Kázmér, Miklós},
	doi = {10.33736/jbk.5110.2022},
	journal-iso = {JBK},
	journal = {Journal of Borneo-Kalimantan},
	volume = {8},
	unique-id = {33542592},
	issn = {2289-2583},
	abstract = {Theodor Posewitz, a Hungarian medical doctor and geologist (1850–1917) spent five years in the Dutch East Indies between 1880 and 1885, serving the colonial Dutch army. During his service assignments he spent all his free time with geological exploration, ultimately yielding the first geological map and monograph of Borneo. Being a citizen of Hungary, a country without any colonial aspirations, he was able to observe, investigate both nature and people of the region without relying to conventional prejudices of colonial officers. His description of Banjarmasin – published originally in Hungarian – is a prime example of objective, impartial, scientific description of land and people; a valuable source to the geography, public health and social structure of the town back in 1887. A list of scientific publications of Posewitz on the East Indies is added in the Appendix.},
	year = {2022},
	pages = {1-6},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:33263577,
	title = {Geoheritage Potential of Miliolite Formation of the Southern Saurashtra (Western India), Gujarat},
	url = {https://m2.mtmt.hu/api/publication/33263577},
	author = {Prizomwala, S. P. and Tandon, Aashna and Kázmér, Miklós and Makwana, Nisarg and Solanki, Tarun and Chauhan, Gaurav},
	doi = {10.1007/s12371-022-00761-1},
	journal-iso = {GEOHERITAGE},
	journal = {GEOHERITAGE},
	volume = {14},
	unique-id = {33263577},
	issn = {1867-2477},
	abstract = {The paper introduces the transboundary approach for landscape geointerpretation using a karst landscape (NW Dinaric Karst) as an example. It proposes geointerpretation that focuses on attractive geoheritage themes that are unique to a karst landscape, such as “duality” of the landscape (surface and underground landscape), geodiversity and geohistory of explorations. Four representative karst landscape types are presented in two neighbouring countries, Slovenia (SI) and Croatia (HR): low karst (Karst Plateau/SI), contact karst (UNESCO site Škocjan Caves/ SI), high alpine glacial karst (Gorski Kotar/HR) and coastal karst (Island of Krk/HR). The transboundary geointerpretation approach is based on an interpretive planning process, which was conducted through participatory workshops with local people and stakeholders and resulted in one interpretive master plan and four permanent exhibition plans. The key phenomena and themes for permanent exhibition plans were identified and used as the basis for the establishment of off-site karst interpretive centres and on-site polygons. The karst heritage was interpreted by using Freeman Tilden’s basic principles of interpretation. The presented approach and the interpretive infrastructure provide a good basis for further geoconservation projects, as well as for geopark designation. Its transferability and further geotourism applications are discussed.},
	year = {2022},
	eissn = {1867-2485},
	pages = {1-13},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@inproceedings{MTMT:33152993,
	title = {Was Antiquity seismically more active than the Middle Ages? - Roman earthquakes in Pannonia and Dacia},
	url = {https://m2.mtmt.hu/api/publication/33152993},
	author = {Kázmér, Miklós and Győri, Erzsébet and Gaidzik, Krysztof},
	booktitle = {Proceedings of the Third European Conference on Earthquake Engineering and Seismology - 3ECEES},
	unique-id = {33152993},
	year = {2022},
	pages = {4467-4476},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}