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Data · dataset · 2026

Provenance and Metallogenic Evolution of the Zhungeer Bauxite Series, Inner Mongolia :Constraints from Detrital Zircon and Rutile Geochronology

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Table 1 shows the analysis results of detrital zircon U-Pb and trace elements in the Upper Carboniferous Benxi Formation bauxite series and overlying sandstone layers in Zhungeer, Inner Mongolia.

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Table 2 shows the analysis results of detrital zircon Lu Hf in the Upper Carboniferous Benxi Formation bauxite series and overlying sandstone layers in Zhungeer, Inner Mongolia. Table 3 shows the analysis results of detrital zircon U-Pb and trace elements in the Upper Carboniferous Benxi Formation bauxite series and overlying sandstone layers in Zhungeer, Inner Mongolia.

Table 4 shows the analysis results of major and trace elements in the Upper Carboniferous Benxi Formation bauxite series in Zhungeer, Inner Mongolia U-Pb dating of detrital zircons and hematites, and Hf isotope data of detrital zircons were obtained using LA-ICP-MS method. Data processing was completed using ICPMSDataCal and Isoplot software. Some sample numbers were missing due to not being measured or the data quality did not meet the requirements.

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Hf analysis is only for representative zircon particles and does not constitute data loss; The whole rock geochemical data were determined by XRD and ICP-MS, and a total of 61 indicators were measured for the major elements (wt%) and trace elements (ppm) of three whole rock samples. The accuracy of whole rock analysis is better than ± 1% -2% for major elements and ± 5% -10% for trace elements. 

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Geology 71% · Tabular 65%
Provenance · 1 source records, 12 field assertions
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ScienceDB10.57760/sciencedb.cjxb.000139 d agoJSON v1
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