TY  - JOUR
AU  - Słodczyk, E
AU  - Pietranik, A
AU  - Repstock, A
AU  - Przybyło, A
AU  - Glynn, S
AU  - Haranginé Lukács, Réka
TI  - Zircon trace element fingerprint of changing tectonic regimes in Permian rhyolites from the Central European Lowlands
JF  - INTERNATIONAL JOURNAL OF EARTH SCIENCES
J2  - INT J EARTH SCI
VL  - In press
PY  - 2024
SN  - 1437-3254
DO  - 10.1007/s00531-024-02419-5
UR  - https://m2.mtmt.hu/api/publication/34853974
ID  - 34853974
AB  - The late Carboniferous/early Permian post-collisional rhyolites (305–285 Ma) that formed in Central Europe have generally similar whole rock compositions to that of older Late-Variscan rhyolites (330–310 Ma). However, data compilation combining zircon age with the chemical composition of rhyolites from 20 units shows a trend of increasing zircon saturation temperature with decreasing age. This trend is particularly well identified in rhyolites from the Central European Lowlands (CEL)—consisting of the NE German and NW Polish Basin—and also correlates their location with the zircon saturation temperature increasing from SE to NW from 750°C to 850°C. We infer that these higher temperatures of zircon saturation reflect a contemporaneous change in the tectonic setting from collisional to divergent, reflecting the onset of the Central European continental rifting. This interpretation is further corroborated by the trace element compositions of the CEL zircons, which resembles zircon crystallized in a divergent setting. Interestingly, the zircon formed globally in this type of setting is chemically diverse, especially considering uranium concentration. For example, zircon from locations dominated by mafic magma fractionation, such as rhyolites from Iceland, have low U concentrations and low U/Yb ratios. On the other hand, zircon formed in rhyolites in rifted margins, like western North America, tends to have much higher U and U/Yb ratios. Such high concentrations are not observed in zircon from the CEL, suggesting that the mantle input could be higher and residence times within continental crust shorter than those for rhyolites from the Cenozoic western USA. This may, in turn, suggest that the region might have been affected by a hot spot, similar to that responsible for rhyolite formation of the Snake River Plain.
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Rinyu, László
AU  - Czébely, Andrea
AU  - Kiss, D
AU  - Kele, Sándor
AU  - Túri, Marianna
TI  - Improving the long-term Δ47 reproducibility of the Thermo Scientific 253 Plus 10 kV IRMS using a prototype Peltier cooling device
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
PG  - 1
DO  - 10.5194/egusphere-egu24-10068
UR  - https://m2.mtmt.hu/api/publication/34834799
ID  - 34834799
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Kaushal, N
AU  - Lechleitner, FA.
AU  - Wilhelm, M
AU  - Azennoud, K
AU  - Bühler, JC.
AU  - Braun, K
AU  - Ait Brahim, Y
AU  - Baker, A
AU  - Burstyn, Y
AU  - Comas-Bru, L
AU  - Fohlmeister, J
AU  - Goldsmith, Y
AU  - Harrison, SP.
AU  - Hatvani, István Gábor
AU  - Rehfeld, K
AU  - Ritzau, M
AU  - Skiba, V
AU  - Stoll, HM.
AU  - Szűcs, József Gábor
AU  - Tanos, Péter
AU  - Treble, PC.
AU  - Azevedo, V
AU  - Baker, JL.
AU  - Borsato, A
AU  - Chawchai, S
AU  - Columbu, A
AU  - Endres, L
AU  - Hu, J
AU  - Kern, Zoltán
AU  - Kimbrough, A
AU  - Koç, K
AU  - Markowska, M
AU  - Martrat, B
AU  - Masood Ahmad, S
AU  - Nehme, C
AU  - Novello, VF
AU  - Pérez-Mejías, C
AU  - Ruan, J
AU  - Sekhon, N
AU  - Sinha, N
AU  - Tadros, CV.
AU  - Tiger, BH.
AU  - Warken, S
AU  - Wolf, A
AU  - Zhang, H
TI  - SISALv3: a global speleothem stable isotope and trace element database
JF  - EARTH SYSTEM SCIENCE DATA
J2  - EARTH SYST SCI DATA
VL  - 16
PY  - 2024
IS  - 4
SP  - 1933
EP  - 1963
PG  - 31
SN  - 1866-3508
DO  - 10.5194/essd-16-1933-2024
UR  - https://m2.mtmt.hu/api/publication/34823532
ID  - 34823532
AB  - Abstract. Palaeoclimate information on multiple climate variables at different spatiotemporal scales is becoming increasingly important to understand environmental and societal responses to climate change. A lack of high-quality reconstructions of past hydroclimate has recently been identified as a critical research gap. Speleothems, with their precise chronologies, widespread distribution, and ability to record changes in local to regional hydroclimate variability, are an ideal source of such information. Here, we present a new version of the Speleothem Isotopes Synthesis and AnaLysis database (SISALv3), which has been expanded to include trace element ratios and Sr isotopes as additional, hydroclimate-sensitive geochemical proxies. The oxygen and carbon isotope data included in previous versions of the database have been substantially expanded. SISALv3 contains speleothem data from 365 sites from across the globe, including 95 Mg/Ca, 85 Sr/Ca, 52 Ba/Ca, 25 U/Ca, 29 P/Ca, and 14 Sr-isotope records. The database also has increased spatiotemporal coverage for stable oxygen (892) and carbon (620) isotope records compared with SISALv2 (which consists of 673 and 430 stable oxygen and carbon records, respectively). Additional meta information has been added to improve the machine-readability and filtering of data. Standardized chronologies are included for all new entities along with the originally published chronologies. Thus, the SISALv3 database constitutes a unique resource of speleothem palaeoclimate information that allows regional to global palaeoclimate analyses based on multiple geochemical proxies, permitting more robust interpretations of past hydroclimate and comparisons with isotope-enabled climate models and other Earth system and hydrological models. The database can be accessed at https://doi.org/10.5287/ora-2nanwp4rk (Kaushal et al., 2024).
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Cseresznyés, Dóra
AU  - Preto, N
AU  - Báldi, Katalin
AU  - Kónya, Péter
AU  - Király, Csilla
AU  - Gelencsér, Orsolya
AU  - Szamosfalvi, Ágnes
AU  - Szabó, Csaba
AU  - Czuppon, György
AU  - Falus, György
TI  - Limestone reservoirs: are they good for CO2 geological storage?
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-12575
UR  - https://m2.mtmt.hu/api/publication/34821362
ID  - 34821362
N1  - poszter
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Király, Csilla
AU  - Keya, Mondal J
AU  - Jakab, Gergely Imre
AU  - Karlik, Máté
AU  - Falus, György
AU  - Cseresznyés, Dóra
AU  - Kónya, Péter
AU  - Viczián, István
AU  - Szeberényi, József
AU  - Szalai, Zoltán
TI  - Varying weathering degree indicators within three paleosol layers
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-11217
UR  - https://m2.mtmt.hu/api/publication/34821344
ID  - 34821344
N1  - poszter
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Salcher, B
AU  - Neuhuber, S
AU  - Otto, JC
AU  - Payer, T
AU  - Lüthgens, C
AU  - Fuchs, S
AU  - Flores-Orozco, A
AU  - Ruszkiczay-Rüdiger, Zsófia
AU  - Grupe, S
AU  - Fiebig, M
TI  - River terrace formation in response to climate, regional uplift and local normal faulting: The Danube terrace staircase in Vienna
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-10609
UR  - https://m2.mtmt.hu/api/publication/34806058
ID  - 34806058
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Telbisz, Tamás Ferenc
AU  - Krasznai, M
AU  - Gachev, E
AU  - Gikov, A
AU  - Ruszkiczay-Rüdiger, Zsófia
TI  - Glacial cirque morphometry of Rila and Pirin Mountains (Bulgaria)
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-20311
UR  - https://m2.mtmt.hu/api/publication/34805900
ID  - 34805900
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Perșoiu, I
AU  - Cruceru, N
AU  - Rădoane, M
AU  - Preoteasa, L
AU  - Ruszkiczay-Rüdiger, Zsófia
TI  - Quaternary evolution of the Danube along Lower Danube Gorge (Iron Gates) and Oltenia Plain (Romania, SE Europe) – a literature review
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-15722
UR  - https://m2.mtmt.hu/api/publication/34805888
ID  - 34805888
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Ruszkiczay-Rüdiger, Zsófia
AU  - Kern, Zoltán
AU  - Madarász, Balázs
AU  - Urdea, P
AU  - Braucher, R
AU  - Molnár, Mihály
AU  - Buró, Botond
ED  - Team, A / Collaborative Organization
TI  - New surface exposure age data using cosmogenic radionuclides 10Be and 14C to constrain the age of the last deglaciation in the Retezat Mts, Southern Carpathians, Romania
T2  - EGU General Assembly 2024 : abstracts
PB  - European Geosciences Union (EGU)
C1  - Wien
PY  - 2024
DO  - 10.5194/egusphere-egu24-12758
UR  - https://m2.mtmt.hu/api/publication/34805880
ID  - 34805880
N1  - poszter
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Saeed, Bidar Kahnamuei
AU  - Hegedűs-Csondor, Katalin
AU  - Baják, Petra
AU  - Horváth, Ákos
AU  - Szieberth, Dénes
AU  - Czuppon, György
AU  - Vargha, Márta
AU  - Izsák, Bálint
AU  - Németh, György
AU  - Tóth, György
AU  - Erőss, Anita
TI  - Application of natural radionuclides in the hydrogeological characterization of karst system supplying the Lake Hévíz
T2  - 54. Ifjú Szakemberek Ankétja Absztraktkötet - LIV. Meeting of Young Geoscientists Book of Abstracts
PY  - 2024
SP  - 50
EP  - 51
PG  - 1
UR  - https://m2.mtmt.hu/api/publication/34804501
ID  - 34804501
LA  - English
DB  - MTMT
ER  -