The provenance of Danubian loess

被引:27
作者
Fenn, Kaja [1 ,2 ]
Millar, Ian L. [3 ]
Durcan, Julie A. [2 ]
Thomas, David S. G. [2 ]
Banak, Adriano [4 ]
Markovic, Slobodan B. [5 ]
Veres, Daniel [6 ]
Stevens, Thomas [7 ]
机构
[1] Univ Liverpool, Dept Geog & Planning, Liverpool L69 7ZT, Merseyside, England
[2] Univ Oxford, Ctr Environm, South Parks Rd, Oxford OX1 3QY, England
[3] British Geol Survey, Geochronol & Tracers Facil, Keyworth NG12 5GG, Notts, England
[4] Croatian Geol Survey, Dept Geol, Sachsova 2, HR-10000 Zagreb, Croatia
[5] Univ Novi Sad, Fac Sci, Trg Dositeja Obradov 3, Novi Sad 21000, Serbia
[6] Romanian Acad, Inst Speleol, Clinicilor 5, Cluj Napoca 400006, Romania
[7] Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden
基金
瑞典研究理事会;
关键词
Geochronology; U-Pb; Hf isotopes; Quaternary; Loess-palaeosol sequences; Aeolian; Zircon; Fluvial; PERI-GONDWANAN TERRANES; EAST-AFRICAN OROGEN; SIZED QUARTZ SILT; U-PB AGES; GRAIN-SIZE; LU-HF; DETRITAL ZIRCON; CENTRAL-EUROPE; DESERT LOESS; PAN-AFRICAN;
D O I
10.1016/j.earscirev.2022.103920
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Fenn, K., Durcan, J.A., Thomas, D.S.G., Banak, A., 2020a. A 180 ka record of environmental change at Erdut (Croatia): a new chronology for the loess-palaeosol sequence and its implications for environmental interpretation. J. Quat. Sci. 35, 582-593. https://doi.org/10.1002/jqs.3201.
引用
收藏
页数:22
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