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REE Tetrad Effect as a Powerful Indicator of Formation Conditions of Karst Bauxites: A Case Study of the Shahindezh Deposit, NW Iran
Author(s) -
ABEDINI Ali,
REZAEI AZIZI Mansour,
CALAGARI Ali Asghar
Publication year - 2019
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.13763
Subject(s) - tetrad , bauxite , geology , sedimentary depositional environment , mineralogy , karst , geochemistry , alkali metal , chemistry , geomorphology , mathematics , paleontology , organic chemistry , structural basin , mathematical physics
Study of the concentration of major, trace, and rare earth elements (REE) in the Shahindezh karst bauxite deposit, northwestern Iran clarifies the relationship of the tetrad effect with geochemical parameters in the bauxite ores. The existence of irregular curves in the chondrite‐normalized REE patterns as well as non‐CHARAC behavior of geochemically isovalent pairs (Y/Ho) are related to the tetrad effect. The meaningful positive correlation between the sizes of the calculated T 3 tetrad effect and some geochemical factors such as Y/Ho, ΣREE, La/Y, (La/Yb) N , and (LREE/HREE) N as well as some major oxides‐based parameters like Al 2 O 3 + LOI/SiO 2 + Fe 2 O 3 , Al 2 O 3 /Fe 2 O 3 , Al 2 O 3 + LOI, IOL, and SiO 2 + Fe 2 O 3 indicate that the studied bauxite horizon was likely deposited by different (acidic and/or alkalic) solutions at different stages. The lower part of the studied horizon with a thickness of ∼4.7 m displays alkali characteristics whereas the upper parts of the horizon with a thickness of ∼5.3 m are characterized by more acidic conditions. These results are fully supported by the co‐occurrence of convex‐concave tetrad effect curves in the chondrite‐normalized REE patterns. Therefore, the tetrad effect phenomenon used in this study has proved to be a good and reliable geochemical proxy to assess the conditions of the depositional environment in the Shahindezh bauxite ores.