THE PERMIAN ALKALINE GRANITES IN CENTRAL INNER MONGOLIA AND THEIR GEODYNAMIC SIGNIFICANCE
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Abstract:
Alkaline granites (Rb-Sr ages 276-286 Ma) occurring in the Bayan Ul-Dong Ujimqin belt at the south margin of the Siberian plate, and generated under tension-al tectonic enviroments, are about 60Ma younger than the Late Devonian to Early Carboniferous coll
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Hong Dawei, Huang Huaizeng Xiao Yijun Xu Haiming.1994. THE PERMIAN ALKALINE GRANITES IN CENTRAL INNER MONGOLIA AND THEIR GEODYNAMIC SIGNIFICANCE[J]. Acta Geologica Sinica,68(3):
