@article{MTMT:34654694, title = {Loess origin and late Pleistocene environmental reconstruction for northeastern Iran : multiproxy evidences from the Chenarli loess-paleosol sequence}, url = {https://m2.mtmt.hu/api/publication/34654694}, author = {Ghafarpour, A and Khormali, F and Tazikeh, H and Kehl, M and Frechen, M and Zolitschka, B}, doi = {10.1016/j.quascirev.2024.108545}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {328}, unique-id = {34654694}, issn = {0277-3791}, year = {2024}, eissn = {1873-457X}, orcid-numbers = {Ghafarpour, A/0000-0002-9170-9386; Zolitschka, B/0000-0001-8256-0420} } @article{MTMT:34782030, title = {The indicative significance of grain size end-members and quartz surface microtextural features in Beglitsa loess sections at the Sea of Azov}, url = {https://m2.mtmt.hu/api/publication/34782030}, author = {Liang, Y and Yang, T and Wang, L and Shi, P and Matishovc, GG. and Velichko, AA. and Zeng, B}, doi = {10.1016/j.aeolia.2024.100921}, journal-iso = {AEOLIAN RES}, journal = {AEOLIAN RESEARCH}, volume = {67-69}, unique-id = {34782030}, issn = {1875-9637}, year = {2024}, eissn = {2212-1684} } @article{MTMT:34578081, title = {Source areas and paleoenvironmental reconstruction of the Serra d'Almenara loess (NE Ebro Valley, Iberian Peninsula) from grain-size and heavy mineral signatures}, url = {https://m2.mtmt.hu/api/publication/34578081}, author = {Plata, JM. and Balasch, JC and Boixadera, J and Baltiérrez, A and Preusser, F and Poch, RM.}, doi = {10.1016/j.geomorph.2024.109085}, journal-iso = {GEOMORPHOLOGY}, journal = {GEOMORPHOLOGY}, volume = {451}, unique-id = {34578081}, issn = {0169-555X}, year = {2024}, eissn = {1872-695X} } @article{MTMT:34501630, title = {Evolution of the Asian monsoon recorded by Holocene aeolian sediments in the northeastern Tibetan Plateau}, url = {https://m2.mtmt.hu/api/publication/34501630}, author = {Xu, A and Hu, M and Bai, Q}, doi = {10.1016/j.jseaes.2024.106021}, journal-iso = {J ASIAN EARTH SCI}, journal = {JOURNAL OF ASIAN EARTH SCIENCES}, volume = {263}, unique-id = {34501630}, issn = {1367-9120}, year = {2024}, eissn = {1878-5786} } @article{MTMT:34094128, title = {Improving Grain Size Analysis to Characterize Sedimentary Processes in a Low-Energy River: A Case Study of the Charente River (Southwest France)}, url = {https://m2.mtmt.hu/api/publication/34094128}, author = {Duquesne, A and Carozza, JM}, doi = {10.3390/app13148061}, journal-iso = {APPL SCI-BASEL}, journal = {APPLIED SCIENCES-BASEL}, volume = {13}, unique-id = {34094128}, abstract = {The recognition and quantification of fluvial transport and depositional processes has widely been studied. However, few works have focused on the interpretation and quantification of sedimentary processes in low-energy fluvial environments. This paper features and compares the results of five methods of grain size data processing (statistic moments, textural analysis, multivariate statistics combining Principal Component Analysis and hierarchical cluster analysis, and CM image and end-member modeling analysis) and discusses their efficiencies in characterizing low-energy alluvial plain deposits. These environments are characterized by fine grain size, high-homogeneity deposits at the macroscopic scale, and low grain size variability, hence presenting a difficulty in identifying and splitting an apparently homogeneous sedimentary record into sedimentary sequences. These statistical methods are applied on a ~9 m long core extracted from the fluvial island of la Baine located in the downstream section of the Charente River (Chaniers, Charente-Maritime, France). In the light of these results, elementary statistical parameters (statistical moments, modes, and sorting index) have limited interest in the sedimentary description and interpretation of fine fluvial deposits. Textural analyses are more informative but highly dependent on the classification scheme. Only the multivariate statistics approach and end-member modeling analysis present interesting results and allow the robust identification of sub-units. However, multivariate statistics results are dependent on the choice of input variables and do not support non-zero values, while the second method, the most recent and complex one, needs further developments to clearly connect end-member classes to sedimentary processes.}, year = {2023}, eissn = {2076-3417} } @article{MTMT:33777210, title = {Characterization and mapping of MIS‐2 thermal contraction crack polygons in Western Transdanubia, Hungary}, url = {https://m2.mtmt.hu/api/publication/33777210}, author = {Farkas, Beáta and Sipos, György and Bartyik, Tamás and Józsa, Edina and Czigány, Szabolcs and Balogh, Richárd and Varga, Gábor and Kovács, János and Fábián, Szabolcs Ákos}, doi = {10.1002/ppp.2190}, journal-iso = {PERMAFROST PERIGLAC}, journal = {PERMAFROST AND PERIGLACIAL PROCESSES}, volume = {34}, unique-id = {33777210}, issn = {1045-6740}, year = {2023}, pages = {417-427}, orcid-numbers = {Farkas, Beáta/0000-0002-7026-8980; Sipos, György/0000-0001-6224-2361; Czigány, Szabolcs/0000-0002-9158-3162; Kovács, János/0000-0001-7742-5515; Fábián, Szabolcs Ákos/0000-0001-9127-2113} } @article{MTMT:34093218, title = {Morphological analysis of mineral grains from different sedimentary environments using automated static image analysis}, url = {https://m2.mtmt.hu/api/publication/34093218}, author = {Gresina, Fruzsina and Farkas, Beáta and Fábián, Szabolcs Ákos and Szalai, Zoltán and Varga, György}, doi = {10.1016/j.sedgeo.2023.106479}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {455}, unique-id = {34093218}, issn = {0037-0738}, year = {2023}, eissn = {1879-0968}, orcid-numbers = {Farkas, Beáta/0000-0002-7026-8980; Fábián, Szabolcs Ákos/0000-0001-9127-2113; Szalai, Zoltán/0000-0001-5267-411X; Varga, György/0000-0003-4784-6372} } @article{MTMT:33722821, title = {Loess or lake sediments: Resolving the origin of massive beds in the Lower Jurassic of southern Africa}, url = {https://m2.mtmt.hu/api/publication/33722821}, author = {Head, HV. and Bordy, EM.}, doi = {10.1002/gj.4695}, journal-iso = {GEOL J}, journal = {GEOLOGICAL JOURNAL}, volume = {58}, unique-id = {33722821}, issn = {0072-1050}, year = {2023}, eissn = {1099-1034}, pages = {1822-1843}, orcid-numbers = {Head, HV./0000-0002-4808-7104; Bordy, EM./0000-0003-4699-0823} } @article{MTMT:33834227, title = {Universal decomposition model : an efficient technique for palaeoenvironmental reconstruction from grain‐size distribution}, url = {https://m2.mtmt.hu/api/publication/33834227}, author = {Liu, Y and Wang, T and Liu, B and Long, Y and Liu, X and Sun, Y}, doi = {10.1111/sed.13115}, journal-iso = {SEDIMENTOLOGY}, journal = {SEDIMENTOLOGY}, volume = {70}, unique-id = {33834227}, issn = {0037-0746}, year = {2023}, eissn = {1365-3091}, pages = {2127-2149} } @article{MTMT:33678550, title = {End-member characteristics of sediment grain size in modern Yellow River delta sediments and its environmental significance}, url = {https://m2.mtmt.hu/api/publication/33678550}, author = {Meng, L and Wang, L and Zhao, J and Zhan, C and Liu, X and Cui, B and Zeng, L and Wang, Q}, doi = {10.3389/fmars.2023.1141187}, journal-iso = {FRONT MAR SCI}, journal = {FRONTIERS IN MARINE SCIENCE}, volume = {10}, unique-id = {33678550}, year = {2023}, eissn = {2296-7745} } @article{MTMT:34398455, title = {End-member characteristics of sediment grain size of modern Yellow River Delta sediments and their response to channel shifts and human activitie}, url = {https://m2.mtmt.hu/api/publication/34398455}, author = {Meng, L and Wang, L and Zhan, C and Liu, X and Wang, Q}, doi = {10.16028/j.1009-2722.2022.202}, journal = {Marine Geology Letters}, volume = {39}, unique-id = {34398455}, issn = {1009-2722}, year = {2023}, pages = {16-24} } @article{MTMT:33712422, title = {Potential dust sources for loess deposits in Central Italy: A geochemical case study from the Loess-Paleosol-Sequence of Ponte Crispiero (Marche)}, url = {https://m2.mtmt.hu/api/publication/33712422}, author = {Pasquetti, F and Zanchetta, G and Bini, M and Paffi, J and Coltorti, M and Lezzerini, M and Arienzo, I and Cremaschi, M}, doi = {10.1016/j.catena.2023.107064}, journal-iso = {CATENA}, journal = {CATENA}, volume = {226}, unique-id = {33712422}, issn = {0341-8162}, year = {2023}, eissn = {1872-6887} } @article{MTMT:33637948, title = {Single-sample unmixing and parametric end-member modelling of grain-size distributions with transformed probability density functions and their performance comparison using aeolian sediments}, url = {https://m2.mtmt.hu/api/publication/33637948}, author = {Peng, J and Wang, X and Zhao, H and Dong, Z}, doi = {10.1016/j.sedgeo.2022.106328}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {445}, unique-id = {33637948}, issn = {0037-0738}, year = {2023}, eissn = {1879-0968} } @article{MTMT:33904179, title = {Comparison and significance of grain size parameters of the Menyuan loess calculated using different methods}, url = {https://m2.mtmt.hu/api/publication/33904179}, author = {Shi, Y and Chongyi, E. and Zhang, Z and Peng, Q and Zhang, J and Yan, W and Xu, C}, doi = {10.1515/geo-2022-0474}, journal-iso = {OPEN GEOSCI}, journal = {OPEN GEOSCIENCES}, volume = {15}, unique-id = {33904179}, issn = {2391-5447}, abstract = {Grain size is a fundamental physical property of sediments, and its parameters are crucial indicators of the provenance, transport processes, and depositional environments. However, owing to the availability of graphic and moment method choices for the determination of grain size parameters, the associated data are characterized by inconsistencies, and these issues restrict the utilization of such data. Compared to other regions, comparative analyses of grain size parameters determined using the graphic and moment methods for aeolian sediments in the Tibetan Plateau are scant. To obtain more accurate information and optimize and integrate historical data, in the present study, sediments in the Yahecun section of the Menyuan Basin in the northeastern Tibetan Plateau were investigated. Data for the Menyuan loess show that the mean grain size, sorting, skewness, and kurtosis data obtained from the two methods can be converted using linear equations. However, differences in the descriptions following the establishment of relationships should be considered. Owing to its sedimentary characteristics, the moment method is more suitable for determining grain size parameters for the Menyuan loess. The results from the moment method indicate that the Menyuan loess originated from multiple sources involving varying dynamics, and the sediments recorded changes from a cold, dry to a warm climate.}, keywords = {graphic method; Moment method; Menyuan Basin; Grain size parameters; aeolian loess}, year = {2023}, eissn = {2391-5447} } @article{MTMT:34224817, title = {Comparative analysis of grain size end member of Harbin loess and climatic significance}, url = {https://m2.mtmt.hu/api/publication/34224817}, author = {Song, Y and CHI, Y and Xie, Y and Kang, C and Wei, Z and Wu, P and Sun, L and Liu, R}, doi = {10.18306/dlkxjz.2023.09.013}, journal-iso = {PROGRESS GEOGRAPHY}, journal = {PROGRESS IN GEOGRAPHY}, volume = {42}, unique-id = {34224817}, issn = {1007-6301}, year = {2023}, pages = {1825-1840} } @CONFERENCE{MTMT:34158236, title = {LÖSZ ÜLEDÉKEK ELTERJEDÉSE, KIALAKULÁSA, FIZIKAI JELLEMZŐI, ÁSVÁNYOS ÉS GEOKÉMIAI ÖSSZETÉTELE: ANYAGVIZSGÁLATOKTÓL A PALEOKLÍMA REKONSTRUKCIÓKIG}, url = {https://m2.mtmt.hu/api/publication/34158236}, author = {Újvári, Gábor}, booktitle = {13. Kőzettani és Geokémiai Vándorgyűlés}, unique-id = {34158236}, year = {2023}, pages = {27-29}, orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155} } @inbook{MTMT:31836829, title = {7.13 - Dust deposits: loess}, url = {https://m2.mtmt.hu/api/publication/31836829}, author = {Fenn, K and Prud’Homme, C}, booktitle = {Treatise on Geomorphology}, doi = {10.1016/B978-0-12-818234-5.00028-6}, unique-id = {31836829}, year = {2022}, pages = {320-365} } @article{MTMT:32596596, title = {The provenance of Danubian loess}, url = {https://m2.mtmt.hu/api/publication/32596596}, author = {Fenn, K and Millar, I L and Durcan, J A and Thomas, D S G and Banak, A and Marković, S B and Veres, D and Stevens, Th}, doi = {10.1016/j.earscirev.2022.103920}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {226}, unique-id = {32596596}, issn = {0012-8252}, year = {2022}, eissn = {1872-6828} } @article{MTMT:32959336, title = {Investigating Potential Links Between Fine-Grained Components in Loess and Westerly Airflow: Evidence From East and Central Asia}, url = {https://m2.mtmt.hu/api/publication/32959336}, author = {Li, Y and Song, Y and Fitzsimmons, KE and Dave, AK and Liu, Y and Zong, X and Sun, H and Liu, H and Orozbaev, R}, doi = {10.3389/feart.2022.901629}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {10}, unique-id = {32959336}, abstract = {Loess is a ubiquitous, silty aeolian sediment common across the semiarid to subhumid regions in the Northern Hemisphere. As such, the physical characteristics of loess sediment, such as modal grain size and quartz crystallinity index, have the potential to inform us about dust transport pathways and corresponding atmospheric circulation responsible for entrainment, transport, and deposition. In this article, we combine detailed granularity analyses and non-parametric end-member modeling with investigations of the quartz crystallinity index of three loess deposits, extending from East to Central Asia, with the aim of identifying dust transport processes and the climate subsystems responsible for them. We find marked differences in the grain size characteristics of Eastern and Central Asian loess. Given potential linkages of fine particles to the westerly jet stream, here we focused on the fine-grained end-members in the loess. The fine-grained components of the Central Asian Bishkek (BSK) and Chashmanigar (CMG) loess may be derived from individual particles carried at high altitude by major climate subsystems such as the westerlies. However, similar quartz crystallinity indexes of fine- and coarse-grained components in the Central Asian loess indicated that surface-level wind strength might influence the releases from proximal-sourced regions and abundances in the upper atmosphere for the fine particles. By contrast, the fine-grained component of the East Asian [Fanshan18 (FS18)] loess seems to yield physical similarities to the Tertiary Red Clays underlying many loess stratigraphies, and has been interpreted to relate to transport associated with the East Asian winter monsoon. It was further supported by quartz crystallinity indexes of the <16 mu m fractions in the FS18 loess, basically consistent with those of the deserts in North China, highlighting the near-surface northwesterly winter monsoon as the dominant transport dynamics of fine-grained dust. In addition, comparisons of quartz crystallinity indexes of fine-grained components between the East and Central Asian loess also suggest that variations in fine particles within the loess might not be related to transport by the higher-level westerlies, which is in disagreement with the previous model. Therefore, our results indicate that variations in fine-grained end-members in loess are difficult to reliably document the variabilities of higher-level westerlies.}, year = {2022}, eissn = {2296-6463} } @article{MTMT:32783353, title = {Saharan dust deposition in Central Europe in 2016 : a representative year of the increased North African dust removal over the last decade}, url = {https://m2.mtmt.hu/api/publication/32783353}, author = {Rostási, Ágnes and Topa, Boglárka Anna and Gresina, Fruzsina and Weiszburg, Tamás and Gelencsér, András and Varga, György}, doi = {10.3389/feart.2022.869902}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {10}, unique-id = {32783353}, abstract = {Changes in circulation patterns associated with climate change have led to an increase in the frequency and intensity of Saharan dust events (SDEs) in the Carpathian Basin. The annual number of dust events was 4.2 on average between 1979 and 2010, while in the period of 2011–2018, it has increased to 10.3. This study presents a quantitative assessment of wet deposition of dust particles to Lake Balaton (Central Europe) with mineralogical and particle size distribution measurements. In addition to a comprehensive, systematic SDE identification process, rainwater samples were collected in 2016, and the particles on the filters were characterised using a range of analytical techniques. The atmospheric transport of particulates and moisture was evaluated using HYSPLIT Lagrangian trajectory model. XRD measurements revealed that during these events, the major minerals were quartz, kaolinite and 10-Å phyllosilicates. In addition, mineralogical source markers of arid dust (palygorskite and smectite) were also identified in majority of the analysed samples. Based on the results, wet deposition fluxes of dust particles were estimated for the region. 2016 was a typical and representative year for the decade, with twelve identified dust episodes. The synoptic patterns of the events fit well with the typical meteorological character of the North African dust intrusions with enhanced atmospheric meridionality described earlier. From the twelve episodes of 2016, seven were depositional events when wet deposition could be observed at ground level. Dust material of five episodes was analysed in detail, while particles of the two February wet deposition episodes were only granulometrically characterised. General uncertainties that hinder the characterisation of mineral dust in climate models were also observed in the granulometric and dust flux data of the sampled material. The particle size of the deposited dust was coarser than the upper cut-off level of grain size of the models. In addition, the discrepancies between measured and simulated deposition values clearly demonstrated the incorrect representation of dust flux in numerical simulations (partly due to inaccurate grain size data in the models).}, year = {2022}, eissn = {2296-6463}, orcid-numbers = {Rostási, Ágnes/0000-0002-0269-390X; Topa, Boglárka Anna/0000-0003-1996-2261; Weiszburg, Tamás/0000-0001-8183-4434; Gelencsér, András/0000-0003-4563-0295; Varga, György/0000-0003-4784-6372} } @article{MTMT:33144407, title = {A Fractal Entropy-Based Effective Particle Model Used to Deduce Hydraulic Conductivity of Granular Soils}, url = {https://m2.mtmt.hu/api/publication/33144407}, author = {Zhang, G. and Wang, H. and Israr, J. and Ma, W. and Yang, Y. and Ren, K.}, doi = {10.3390/fractalfract6090474}, journal-iso = {FRACTAL FRACT}, journal = {FRACTAL AND FRACTIONAL}, volume = {6}, unique-id = {33144407}, year = {2022}, eissn = {2504-3110} } @article{MTMT:32498312, title = {Dust accumulation process indicated by grain size end-members of the coastal loess since the Late Pleistocene in Miaodao Islands of Shandong Province}, url = {https://m2.mtmt.hu/api/publication/32498312}, author = {Chen, H and Kong, F and Xu, S and Miao, X}, doi = {10.11928/j.issn.1001-7410.2021.05.07}, journal-iso = {QUATERN SCI}, journal = {QUATERNARY SCIENCES}, volume = {41}, unique-id = {32498312}, issn = {1001-7410}, year = {2021}, pages = {1306-316} } @article{MTMT:32546035, title = {Late Pleistocene climate and dust source from the Mobarakabad loess-paleosol sequence, northern foothills of the Alborz Mountains, Northern Iran}, url = {https://m2.mtmt.hu/api/publication/32546035}, author = {Ghafarpour, A and Khormali, F and Meng, X and Tazikeh, H and Stevens, Th}, doi = {10.3389/feart.2021.795826}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {9}, unique-id = {32546035}, year = {2021}, eissn = {2296-6463} } @article{MTMT:31656461, title = {Determining the spatio-temporal response of downstream coarse sediment sorting process in the Chel river (North Bengal, India) using cluster analysis}, url = {https://m2.mtmt.hu/api/publication/31656461}, author = {Ghosh, D and Saha, S}, doi = {10.1007/s40808-020-01028-w}, journal-iso = {MESE}, journal = {MODELING EARTH SYSTEMS AND ENVIRONMENT}, volume = {7}, unique-id = {31656461}, issn = {2363-6203}, year = {2021}, eissn = {2363-6211}, pages = {1353-1372} } @article{MTMT:32528518, title = {Early–Middle Pleistocene Magnetostratigraphic and Rock Magnetic Records of the Dolynske Section (Lower Danube, Ukraine) and Their Application to the Correlation of Loess–Palaeosol Sequences in Eastern and South-Eastern Europe}, url = {https://m2.mtmt.hu/api/publication/32528518}, author = {Hlavatskyi, D and Bakhmutov, V}, doi = {10.3390/quat4040043}, journal-iso = {Quaternary}, journal = {QUATERNARY}, volume = {4}, unique-id = {32528518}, issn = {2571-550X}, year = {2021}, orcid-numbers = {Hlavatskyi, D/0000-0002-9901-7827} } @article{MTMT:32052651, title = {New insights into loess formation on the southern margin of the Chinese Loess Plateau}, url = {https://m2.mtmt.hu/api/publication/32052651}, author = {Hou, K and Qian, H and Zhang, Y and Zhang, Q and Qu, W}, doi = {10.1016/j.catena.2021.105444}, journal-iso = {CATENA}, journal = {CATENA}, volume = {204}, unique-id = {32052651}, issn = {0341-8162}, year = {2021}, eissn = {1872-6887} } @article{MTMT:32462817, title = {Analysis of surface morphology of basaltic grains as environmental indicators for Mars}, url = {https://m2.mtmt.hu/api/publication/32462817}, author = {Kapui, Zsuzsanna and Kereszturi, Ákos and Józsa, Sándor and Király, Csilla and Szalai, Zoltán}, doi = {10.1016/j.pss.2021.105338}, journal-iso = {PLANET SPACE SCI}, journal = {PLANETARY AND SPACE SCIENCE}, volume = {208}, unique-id = {32462817}, issn = {0032-0633}, year = {2021}, eissn = {1873-5088}, orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Szalai, Zoltán/0000-0001-5267-411X} } @article{MTMT:31897330, title = {Application of grain size endmember analysis in the study of dust accumulation processes: A case study of loess in Shandong Province, East China}, url = {https://m2.mtmt.hu/api/publication/31897330}, author = {Kong, F and Xu, S and Han, M and Chen, H and Miao, X and Kong, X and Jia, G}, doi = {10.1016/j.sedgeo.2021.105868}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {416}, unique-id = {31897330}, issn = {0037-0738}, abstract = {The accumulation processes of loess in Shandong Province record atmospheric circulation changes in eastern China, which can be used to explore the varying characteristics of the East Asian monsoons and the evolution of the local environment. In this study, parameterized grain size endmember analysis is used to reveal the characteristics of sedimentary dynamics, material sources, and environmental evolution of a loess profile in Focun, Zibo City, Shandong Province, China. Optically stimulated luminescence (OSL) ages of the profile ranged from 3.02 ± 0.45 ka to 100.99 ± 13.58 ka. The grain size components of the sediments in the profile were divided into five endmembers. EM1 represents a mixed clay component of pedogenesis, EM2 represents a fine silt component transported by high-altitude westerlies, EM3 represents material that settled in the form of floating dust, EM4 represents a silt component transported by low-altitude near-source areas, and EM5 represents short-distance suspended materials transported under dust storms. Combined with a low frequency magnetic susceptibility (χlf) and chromaticity (a⁎), the characteristics of grain size endmembers indicate changes in sedimentary environments since the last interglacial (MIS 5). In MIS 5 the winter monsoon accumulation was low, with high accumulation during the summer monsoon, and an unstable climate. In MIS 4 the winter monsoon produced high accumulation, with low accumulation during the summer monsoon, and frequent dust storms. In MIS 3 the winter monsoon accumulation was low, westerly circulation and summer monsoon accumulation were high, and the climate was warm and humid. In MIS 2 the winter monsoon accumulation was high, summer monsoon accumulation was low, and the climate was dry and cold. In MIS 1 the westerly circulation and winter monsoon accumulation were low, summer monsoon accumulation was high, and the climate was warm and wet. This reflects the regional response to global climate change. This study shows that the parametric grain size endmember analysis method is feasible in studying the sedimentary dynamics, material sources and sedimentary environment of loess in Shandong Province.}, keywords = {LATE PLEISTOCENE; Grain size endmember; Loess-paleosol-sequences; Environmental evolution}, year = {2021}, eissn = {1879-0968} } @article{MTMT:31826687, title = {Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation}, url = {https://m2.mtmt.hu/api/publication/31826687}, author = {Lehmkuhl, F and Nett, J and Pötter, S and Schulte, P and Sprafke, T and Jary, Z and Antoine, P and Wacha, L and Wolf, D and Zerboni, A and Hošek, J and Slobodan, Marković and Obreht, I and Sümegi, Pál and Veres, D and Zeeden, C and Boemke, B and Schaubert, V and Viehweger, J and Hambach, U}, doi = {10.1016/j.earscirev.2020.103496}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {215}, unique-id = {31826687}, issn = {0012-8252}, year = {2021}, eissn = {1872-6828}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:32778716, title = {Characterisitics of grain size end members and its environmental significance of aeolian sand/loess sedimentary sequence since L2 in Hengshan, Shaanxi Province}, url = {https://m2.mtmt.hu/api/publication/32778716}, author = {Liu, R and Yue, D and Zhao, J and Su, Z and Shi, H and Wang, X}, doi = {10.12118/j.issn.1000-6060.2021.05.14}, journal-iso = {ARID LAND GEOGRAPHY (in Chinese)}, journal = {GANHANQU DILI ARID LAND GEOGRAPHY}, volume = {44}, unique-id = {32778716}, issn = {1000-6060}, year = {2021}, pages = {1328-1338} } @article{MTMT:32471780, title = {QGrain: An open-source and easy-to-use software for the comprehensive analysis of grain size distributions}, url = {https://m2.mtmt.hu/api/publication/32471780}, author = {Liu, Y and Liu, X and Sun, Y}, doi = {10.1016/j.sedgeo.2021.105980}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {423}, unique-id = {32471780}, issn = {0037-0738}, year = {2021}, eissn = {1879-0968} } @article{MTMT:31866993, title = {Loess‐like dust appearance at 40 Ma in central China}, url = {https://m2.mtmt.hu/api/publication/31866993}, author = {Meijer, N and Dupont‐Nivet, G and Barbolini, N and Woutersen, A and Rohrmann, A and Zhang, Y and Liu, X‐J and Licht, A and Abels, H A and Hoorn, C and Tjallingii, R and Andermann, Ch and Dietze, M and Nowaczyk, N}, doi = {10.1029/2020PA003993}, journal-iso = {PALEOCEANOGR PALEOCL}, journal = {PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY}, volume = {36}, unique-id = {31866993}, issn = {2572-4517}, year = {2021}, eissn = {2572-4525}, orcid-numbers = {Meijer, N/0000-0002-2186-5682; Dupont‐Nivet, G/0000-0001-9905-9739; Barbolini, N/0000-0001-7121-3634; Rohrmann, A/0000-0002-8017-294X; Liu, X‐J/0000-0002-8413-2451; Licht, A/0000-0002-5267-7545; Hoorn, C/0000-0001-5402-6191; Tjallingii, R/0000-0002-9723-3622; Andermann, Ch/0000-0003-0921-8455; Dietze, M/0000-0001-6063-1726} } @article{MTMT:32556089, title = {The characteristic of grain-size in Ejina Basin and associated sedimentary dynamic environmental analysis}, url = {https://m2.mtmt.hu/api/publication/32556089}, author = {Xie, K and Yin, H}, doi = {10.7522/j.issn.1000-694X.2021.00091}, journal-iso = {J DESERT RES}, journal = {JOURNAL OF DESERT RESEARCH}, volume = {41}, unique-id = {32556089}, year = {2021}, eissn = {1000-694X}, pages = {111-119} } @article{MTMT:31615979, title = {Drilling fluids: Presence of hazardous btexs and crystalline silica}, url = {https://m2.mtmt.hu/api/publication/31615979}, author = {Chan, L and Arumugam, N and Thirugnana, ST and Chelliapan, S}, journal-iso = {Journal of Environmental Treatment Techniques : JETT}, journal = {Journal of Environmental Treatment Techniques : JETT}, volume = {8}, unique-id = {31615979}, issn = {2309-1185}, year = {2020}, pages = {1029-1035} } @article{MTMT:31277488, title = {Interpretation of sedimentary subpopulations extracted from grain size distributions in loess deposits at the Sea of Azov, Russia}, url = {https://m2.mtmt.hu/api/publication/31277488}, author = {Chen, J. and Yang, T. and Qiang, M. and Matishov, G.G. and Velichko, A.A. and Zeng, B. and Xu, M. and Shi, P.}, doi = {10.1016/j.aeolia.2020.100597}, journal-iso = {AEOLIAN RES}, journal = {AEOLIAN RESEARCH}, volume = {45}, unique-id = {31277488}, issn = {1875-9637}, year = {2020}, eissn = {2212-1684} } @article{MTMT:31270063, title = {Comparison of pipette method and state of the art analytical techniques to determine granulometric properties of sediments and soils}, url = {https://m2.mtmt.hu/api/publication/31270063}, author = {Gresina, Fruzsina}, doi = {10.15201/hungeobull.69.1.3}, journal-iso = {HUNG GEOGR BULL (2009-)}, journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)}, volume = {69}, unique-id = {31270063}, issn = {2064-5031}, year = {2020}, eissn = {2064-5147}, pages = {27-39} } @article{MTMT:31342357, title = {Plio-Pleistocene dust traps on paleokarst surfaces: a case study from the Carpathian Basin}, url = {https://m2.mtmt.hu/api/publication/31342357}, author = {Kovács, János and Újvári, Gábor and Varga, György and Seelos, K and Szabó, Péter and Dezső, József and Gammoudi, Nadia}, doi = {10.3389/feart.2020.00189}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {8}, unique-id = {31342357}, abstract = {Plio-Pleistocene silt/clay-rich deposits and paleo-karst fissure sediments from sites of the northern and southern parts of the Carpathian Basin were investigated. These materials were supposed to be mixed during transport before being captured in karstified fissures. Evidence that the eolian fissure sediments of Plio-Pleistocene age in the older Triassic-Cretaceous limestones are derived from eolian silt and clay includes compositional and textural matches, especially decreasing grain-size trends observed downwards from the paleo-surface of the former landscape. Various environmental factors could be recognized by the statistical evaluation of grain-size distribution curves of fissure fillings sediments, such as the effects of eolian transport, parent rock type, weathering, and other sediment transport processes. Grain-size distribution curves with a single maximum in the silt size range are typical for the overlying siltstone debris, for the redeposited loess and red paleosol underlying the loess. Red clay fissure fillings yield bimodal grain-size distribution curves with maxima both in the clay and silt fractions. The research reported in this paper identifies for the first time the presence of eolian deposits in karst fissures of the Carpathian Basin and investigates the characteristics and origin.}, year = {2020}, eissn = {2296-6463}, orcid-numbers = {Kovács, János/0000-0001-7742-5515; Újvári, Gábor/0000-0002-2816-6155; Varga, György/0000-0003-4784-6372; Szabó, Péter/0000-0003-0827-3583} } @article{MTMT:31638756, title = {Identifying eolian dust in the geological record}, url = {https://m2.mtmt.hu/api/publication/31638756}, author = {Meijer, N and Dupont-Nivet, G and Licht, A and Trabucho-Alexandre, J and Bourquin, S and Abels, H A}, doi = {10.1016/j.earscirev.2020.103410}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {211}, unique-id = {31638756}, issn = {0012-8252}, year = {2020}, eissn = {1872-6828} } @{MTMT:32800553, title = {Lithology of L1 loess on the northern edge of European loess in the Upper Dnieper River Basin}, url = {https://m2.mtmt.hu/api/publication/32800553}, author = {Mroczek, P and Łanczont, M and Gozhik, P and Komar, M and Nawrocki, J and Hołub, B and Standzikowski, K and Bogucki, A}, booktitle = {Quaternary Stratigraphy – palaeoenvironment, sediments, palaeofauna and human migrations across Central Europe : International conference dedicated to the 70th Birthday Anniversary of prof. Adam Nadachowski}, unique-id = {32800553}, year = {2020}, pages = {90} } @article{MTMT:31270043, title = {Investigation of spectral properties of different Quaternary paleosols and parent materials}, url = {https://m2.mtmt.hu/api/publication/31270043}, author = {Szeberényi, József and Medved’ová, A and Rostinsky, P and Barta, Gabriella and Novothny, Ágnes and Csonka, Diána and Viczián, István and Horváth, Erzsébet and Végh, Tamás}, doi = {10.15201/hungeobull.69.1.1}, journal-iso = {HUNG GEOGR BULL (2009-)}, journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)}, volume = {69}, unique-id = {31270043}, issn = {2064-5031}, year = {2020}, eissn = {2064-5147}, pages = {3-15}, orcid-numbers = {Barta, Gabriella/0000-0002-5460-1085; Novothny, Ágnes/0000-0003-3513-0406; Csonka, Diána/0000-0002-2318-6720; Horváth, Erzsébet/0000-0002-0197-4152; Végh, Tamás/0000-0001-8476-3686} } @mastersthesis{MTMT:32802118, title = {A multi-proxy palaeoenvironmental reconstruction of the Homa Peninsula, Western Kenya}, url = {https://m2.mtmt.hu/api/publication/32802118}, isbn = {9798522949655}, author = {Vincent, T H}, doi = {10.24377/LJMU.t.00014762}, publisher = {Liverpool John Moores University}, unique-id = {32802118}, abstract = {A thesis submitted in partial fulfilment of the requirements of Liverpool John Moores University for the degree of Doctor of Philosophy}, year = {2020} } @article{MTMT:31337645, title = {Progress in Danube Loess and Paleoenvironment Study}, url = {https://m2.mtmt.hu/api/publication/31337645}, author = {Wu, X and Hao, Q and Marković, S and Fu, Y and Namira, Y and Song, Y and Guo, Z}, doi = {10.11867/j.issn.1001-8166.2020.035}, journal-iso = {ADV EARTH SCI}, journal = {DIQIU KEXUE JINZHAN / ADVANCES IN EARTH SCIENCE}, volume = {35}, unique-id = {31337645}, issn = {1001-8166}, year = {2020}, pages = {363-377} } @article{MTMT:31154264, title = {The geomorphology – sediment distribution – soil formation nexus on the northeastern Qinghai-Tibetan Plateau: Implications for landscape evolution}, url = {https://m2.mtmt.hu/api/publication/31154264}, author = {Yang, F. and Zhang, G.-L. and Sauer, D. and Yang, F. and Yang, R.-M. and Liu, F. and Song, X.-D. and Zhao, Y.-G. and Li, D.-C. and Yang, J.-L.}, doi = {10.1016/j.geomorph.2020.107040}, journal-iso = {GEOMORPHOLOGY}, journal = {GEOMORPHOLOGY}, volume = {354}, unique-id = {31154264}, issn = {0169-555X}, year = {2020}, eissn = {1872-695X} } @article{MTMT:30857984, title = {The Lowermost Tejo River Terrace at Foz do Enxarrique, Portugal: A Palaeoenvironmental Archive from c. 60–35 ka and Its Implications for the Last Neanderthals in Westernmost Iberia}, url = {https://m2.mtmt.hu/api/publication/30857984}, author = {Cunha, P and Martins, A and Buylaert, JP and Murray, A and Gouveia, M and Font, E and Pereira, T and Figueiredo, S and Ferreira, C and Bridgland, D and Yang, P and Stevaux, J and Mota, R}, doi = {10.3390/quat2010003}, journal-iso = {Quaternary}, journal = {QUATERNARY}, volume = {2}, unique-id = {30857984}, issn = {2571-550X}, year = {2019} } @article{MTMT:31405995, title = {Grain-size unmixing using the R package EMMAgeo}, url = {https://m2.mtmt.hu/api/publication/31405995}, author = {Dietze, E and Dietze, M}, doi = {10.5194/egqsj-68-29-2019}, journal-iso = {E G QUATERN SCI J}, journal = {EISZEITALTER UND GEGENWART / E&G QUATERNARY SCIENCE JOURNAL}, volume = {68}, unique-id = {31405995}, issn = {0424-7116}, year = {2019}, eissn = {2199-9090}, pages = {29-46} } @mastersthesis{MTMT:32800529, title = {Provenance of late Quaternary loess along the Middle and Lower Danube River, Europe}, url = {https://m2.mtmt.hu/api/publication/32800529}, author = {Fenn, K}, publisher = {University of Oxford}, unique-id = {32800529}, abstract = {Thesis submitted for the degree of Doctor of Philosophy, University of Oxford}, year = {2019} } @article{MTMT:30613177, title = {Loess2M - Modelling and Mapping}, url = {https://m2.mtmt.hu/api/publication/30613177}, author = {Hao, Q. and Zeeden, C. and Moska, P. and Tomić, N.}, doi = {10.1016/j.quaint.2019.02.030}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {502}, unique-id = {30613177}, issn = {1040-6182}, year = {2019}, eissn = {1873-4553}, pages = {1-3} } @article{MTMT:30766303, title = {Atmospheric Dust Variations in the Ili Basin, Northwest China, During the Last Glacial Period as Revealed by a High Mountain Loess‐Paleosol Sequence}, url = {https://m2.mtmt.hu/api/publication/30766303}, author = {Li, Y and Song, Y and Qiang, M and Miao, Y and Zeng, M}, doi = {10.1029/2019JD030470}, journal-iso = {J GEOPHYS RES ATMOS}, journal = {JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES}, volume = {124}, unique-id = {30766303}, issn = {2169-897X}, year = {2019}, eissn = {2169-8996}, pages = {8449-8466}, orcid-numbers = {Song, Y/0000-0003-0064-3260; Miao, Y/0000-0002-5804-2874} } @article{MTMT:30681842, title = {Dust accumulation processes of piedmont loess indicated by grain-size end members in northern Ili Basin}, url = {https://m2.mtmt.hu/api/publication/30681842}, author = {Li, Y. and Song, Y. and Zong, X. and Zhang, Z. and Cheng, L.}, doi = {10.11821/dlxb201901012}, journal-iso = {ACTA GEOGR SIN}, journal = {ACTA GEOGRAPHICA SINICA}, volume = {74}, unique-id = {30681842}, issn = {0375-5444}, year = {2019}, pages = {162-177} } @article{MTMT:30715890, title = {Quantified Effects of Particle Refractive Index Assumptions on Laser Diffraction Analyses of Selected Soils}, url = {https://m2.mtmt.hu/api/publication/30715890}, author = {Pachon, JC. and Kowalski, KR. and Butterick, JK. and Bacon, AR.}, doi = {10.2136/sssaj2018.07.0274}, journal-iso = {SOIL SCI SOC AM J}, journal = {SOIL SCIENCE SOCIETY OF AMERICA JOURNAL}, volume = {83}, unique-id = {30715890}, issn = {0361-5995}, year = {2019}, eissn = {1435-0661}, pages = {518-530} } @{MTMT:30937964, title = {Sedimentology of the lowermost Tejo River terrace upper division, c. 43–35 ka, at Vila Velha de Ródão (eastern Portugal) - interpretation of the environmental and climate conditions}, url = {https://m2.mtmt.hu/api/publication/30937964}, author = {Proença, e Cunha P and Mota, R and Gouveia, M P and Font, E and Yang, P and Stevaux, J C and Frechen, M and Vandenberghe, J}, booktitle = {International Meeting on Paleoclimate: change and adaptation : book of abstracts}, unique-id = {30937964}, year = {2019}, pages = {41-42} } @mastersthesis{MTMT:30937985, title = {Palaeoenvironmental reconstruction on the basis of Quaternary palaeo dune sequences on Fuerteventura}, url = {https://m2.mtmt.hu/api/publication/30937985}, author = {Roettig, Ch-B}, publisher = {TU Dresden}, unique-id = {30937985}, year = {2019} } @article{MTMT:30710244, title = {On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records}, url = {https://m2.mtmt.hu/api/publication/30710244}, author = {Varga, György and Gresina, Fruzsina and Újvári, Gábor and Kovács, János and Szalai, Zoltán}, doi = {10.1016/j.sedgeo.2019.05.011}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {389}, unique-id = {30710244}, issn = {0037-0738}, year = {2019}, eissn = {1879-0968}, pages = {42-53}, orcid-numbers = {Varga, György/0000-0003-4784-6372; Újvári, Gábor/0000-0002-2816-6155; Kovács, János/0000-0001-7742-5515; Szalai, Zoltán/0000-0001-5267-411X} } @article{MTMT:3383047, title = {Laser Diffractometry in the Measurements of Soil and Sediment Particle Size Distribution}, url = {https://m2.mtmt.hu/api/publication/3383047}, author = {Bieganowski, A and Ryżak, M and Sochan, A and Barna, Gyöngyi and Hernádi, Hilda Ágnes and Beczek, M and Polakowski, C and Makó, András}, doi = {10.1016/bs.agron.2018.04.003}, journal-iso = {ADV AGRON}, journal = {ADVANCES IN AGRONOMY}, volume = {151}, unique-id = {3383047}, issn = {0065-2113}, abstract = {The laser diffraction method (LDM) is a relatively new technique that is increasingly used in measurements of the particle size distribution (PSD) of soil and sediments. It has significant advantages (high precision, simple and rapid measurement) but the PSDs obtained by LDM often differ from those obtained with previously used sieve-sedimentation methods (SSMs). The main factors influencing the measurements that use LDM (among others: soil pretreatment, construction of the device settings of the operator, specificity of soil material, and the problem of fulfilling the assumptions of the method) are presented and the problem of comparability with SSM. New areas of investigations using LDM are also discussed. The work concludes with a set of postulates that should be taken into account to standardize LDM and increase the comparability of results, not only with SSMs but also with the PSDs obtained in other laboratories, including the diffractometers deriving from other producers.}, year = {2018}, eissn = {2213-6789}, pages = {215-279}, orcid-numbers = {Barna, Gyöngyi/0000-0003-0967-5015; Makó, András/0000-0002-6169-6393} } @article{MTMT:27650160, title = {Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial distribution and grain-size characterization}, url = {https://m2.mtmt.hu/api/publication/27650160}, author = {Bosq, M and Bertran, P and Degeai, J-P and Kreutzer, S and Queffelec, A and Moine, O and Morin, E}, doi = {10.1016/j.geomorph.2018.06.010}, journal-iso = {GEOMORPHOLOGY}, journal = {GEOMORPHOLOGY}, volume = {318}, unique-id = {27650160}, issn = {0169-555X}, year = {2018}, eissn = {1872-695X}, pages = {250-269} } @article{MTMT:27695419, title = {New evidence for the provenance and formation of loess deposits in the Ili River Basin, Arid Central Asia}, url = {https://m2.mtmt.hu/api/publication/27695419}, author = {Li, Y and Song, Y and Fitzsimmons, KE and Chen, X and Wang, Q and Sun, H and Zhang, Z}, doi = {10.1016/j.aeolia.2018.08.002}, journal-iso = {AEOLIAN RES}, journal = {AEOLIAN RESEARCH}, volume = {35}, unique-id = {27695419}, issn = {1875-9637}, year = {2018}, eissn = {2212-1684}, pages = {1-8} } @inbook{MTMT:30316534, title = {Szemcseméret hatása a lösz-paleotalaj sorozatok reflektancia méréseinek eredményeire}, url = {https://m2.mtmt.hu/api/publication/30316534}, author = {Szeberényi, József and Varga, György}, booktitle = {Földrajzi tanulmányok 2018}, unique-id = {30316534}, year = {2018}, pages = {49-53}, orcid-numbers = {Varga, György/0000-0003-4784-6372} } @article{MTMT:27312991, title = {Grain-size characterization of reworked fine-grained aeolian deposits}, url = {https://m2.mtmt.hu/api/publication/27312991}, author = {Vandenberghe, J and Sun, Y and Wang, X and Abels, H A and Liu, X}, doi = {10.1016/j.earscirev.2017.11.005}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {177}, unique-id = {27312991}, issn = {0012-8252}, year = {2018}, eissn = {1872-6828}, pages = {43-52} } @article{MTMT:3357510, title = {Granulometric characterization of paleosols in loess series by automated static image analysis}, url = {https://m2.mtmt.hu/api/publication/3357510}, author = {Varga, György and Kovács, János and Szalai, Zoltán and Cserháti, Csaba and Újvári, Gábor}, doi = {10.1016/j.sedgeo.2018.04.001}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {370}, unique-id = {3357510}, issn = {0037-0738}, keywords = {SEQUENCE; sediment; Sand; grain size; DEPOSITS; PARTICLE-SHAPE; records; PALEOSOLS; loess; Particle shape; laser diffraction; image analyses; WIND TRANSPORT; QUARTZ SILT GRAINS; GRAIN-SIZE MEASUREMENTS}, year = {2018}, eissn = {1879-0968}, pages = {1-14}, orcid-numbers = {Varga, György/0000-0003-4784-6372; Kovács, János/0000-0001-7742-5515; Szalai, Zoltán/0000-0001-5267-411X; Újvári, Gábor/0000-0002-2816-6155} } @article{MTMT:3394402, title = {Identification of Saharan dust particles in Pleistocene dune sand- paleosol sequences of Fuerteventura (Canary Islands)}, url = {https://m2.mtmt.hu/api/publication/3394402}, author = {Varga, György and Roettig, C-B}, doi = {10.15201/hungeobull.67.2.2}, journal-iso = {HUNG GEOGR BULL (2009-)}, journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)}, volume = {67}, unique-id = {3394402}, issn = {2064-5031}, year = {2018}, eissn = {2064-5147}, pages = {121-141}, orcid-numbers = {Varga, György/0000-0003-4784-6372} }