摘要
The Adelagawula syenogranite occurs in Abaga Qi,Inner Mongolia,near the Sino-Mongolian border.The intrusive rock was assigned to Early-Yanshanian(Kγ 5 2)by 1:200 000 regional geological surveyor or Lower Permian as alkali feldspar granite(P 1 χγ)in 1:250 000 regional geological survey.The U-Pb isotopic dating of the syenogranite shows the age of 273.1±0.4 Ma.Combined with regional geological data and previous research,it is possibly a product of Early Permian magmatism.The syenogranite,with high silica,high potassium,per-aluminum and poor calcium-magnesium-iron,belongs to post-orogenic I-type granite.The REE distribution is in V-shaped pattern,with low total rare earth content,unobvious fractionation of LREE and HREE,δEu values ranging from 0.07 to 0.60 and strongly depleted Eu.