SONG Wei-min, XING De-he, GUO Sheng-zhe, PENG Yan-dong, BIAN Xiong-fei, TAO Nan. LITHOGEOCHEMISTRY AND SIGNIFICANCE OF THE XIDUIMIANGOU ROCK BODY IN JINCHANGGOULIANG, INNER MONGOLIA[J]. Geology and Resources, 2009, 18(2): 134-139. DOI: 10.13686/j.cnki.dzyzy.2009.02.004
    Citation: SONG Wei-min, XING De-he, GUO Sheng-zhe, PENG Yan-dong, BIAN Xiong-fei, TAO Nan. LITHOGEOCHEMISTRY AND SIGNIFICANCE OF THE XIDUIMIANGOU ROCK BODY IN JINCHANGGOULIANG, INNER MONGOLIA[J]. Geology and Resources, 2009, 18(2): 134-139. DOI: 10.13686/j.cnki.dzyzy.2009.02.004

    LITHOGEOCHEMISTRY AND SIGNIFICANCE OF THE XIDUIMIANGOU ROCK BODY IN JINCHANGGOULIANG, INNER MONGOLIA

    • Lithogeochemical study shows that the Early Cretaceous Xiduimiangou rock body is typical high-Sr granite, characterized by high Al (14.51% to 16.57% of Al2O3, 15.434% in average), high Na (3.75% to 4.71% of Na2O, 4.313% in average) and high Sr (701×10-6 to 931×10-6 of Sr, averagely 802×10-6) contents, with severe HREE deficiency (21.07-29.13 of (La/Yb)N, 23.54 in average), slightly negative or positive Eu anomalies and rich transitional elements. The rock body is likely related to the thinning of lithosphere in Eastern China. It is importantly significant for the research on the origin of magma in the northern margin of North China Craton.
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