Xie, Yuanyun Yuan, Fang Zhan, Tao Kang, Chunguo Chi, Yunping Ma, Yongfa Provenance discrimination diagrams incorporating REE parameters for the Harbin loess and paleosols. Geochemistry of loess deposits in northeastern China: constraint on provenance and implication for disappearance of the large Songliao palaeolake Supplementary Fig. 4 Provenance discrimination diagrams incorporating REE parameters for the Harbin loess and paleosols. Note that the Harbin dust samples fall within or well close to the field of the Songnen Sandy Land and the Horqin Sandy Land but far outside the field of the Hulun Buir Sandy Land, which reveal that the Harbin aeolian loess sediments have a marked geochemical affinity with the Songnen Sandy Land and the Horqin Sandy Land. Subscript N represents chondrite-normalized values. Eu/Eu* refers to Eu anomaly value equal to Eu<sub>N</sub>/(Sm<sub>N</sub>×Gd<sub>N</sub>)<sup>0.5</sup>. LREE=(La+Ce+Pr+Nd+Sm+Eu); HREE=(Gd+Tb+Dy+Ho+Er+Tm+Yb+Lu); LREE'=(La+Ce+Pr+Nd); HREE'=(Er+Tm+Yb+Lu); MREE=(Sm+Eu+Gd+Tb+Dy+Ho); MREE*=2×MREE/(LREE' + HREE') Chondrite values are after Taylor and McLennan (1985). Harbin loess;Songliao palaeolake Supplementary Fig;Horqin Sandy Land;Eu anomaly value;Harbin dust samples fall;Hulun Buir Sandy Land;Provenance discrimination diagrams;Harbin aeolian loess sediments;MREE;4 Provenance discrimination diagrams;REE parameters;LREE;HREE;Songnen Sandy Land;paleosol;Geology 2017-07-25
    https://geolsoc.figshare.com/articles/figure/Provenance_discrimination_diagrams_incorporating_REE_parameters_for_the_Harbin_loess_and_paleosols_Geochemistry_of_loess_deposits_in_northeastern_China_constraint_on_provenance_and_implication_for_disappearance_of_the_large_Songliao_palaeolake/5240908
10.6084/m9.figshare.5240908.v1