Late Permian monzogranite of Hanggale is characterized by rich alkali metals, poor MgO, TFeO and CaO, enrichment of LREE, and weak negative Eu anomalies, implying an I-type granite. The depletion of Nb, Sr, P, Ti elements shows that such an arc granite has features of intrusive rocks related to subduction. In the R1 -R2 diagram, most of the samples are concentrated along the boundary between the pre-collision granite area and the post-collision granite area. In the Nb-Y diagram, the samples fall into the area of the volcanic arc-syncollisional granite. In the Rb -(Y+Nb)diagram, the samples lie in the area of volcanic arc granite. In the Rb-Hf-Ta diagram, the samples all fall into the arc system. High Th/U ratios in zircon of main rocks show characteristics of magmat-ic zircons; high total REE, heavy REE enrichment and left-oblique curves in the chondnte-normalized diagram are consistent with general characteristics of magmatic zircon distribution. LA-ICP-MS zircon U-Pb dating shows that its age is 253.5±7.9Ma. The Late Permian monzogranite of Hanggale was a pre-collisional volcanic arc granite, and Hanggale area was a volcanic arc that belonged to active continental margin in Late Permian.%杭嘎勒晚二叠世二长花岗岩富碱,贫MgO、TFeO、CaO,轻稀土元素明显富集,具弱负Eu异常,显示Ⅰ型花岗岩的特点.Nb、Sr、P、Ti元素亏损,显示出与俯冲有关的侵入岩特征.在R1-R2图解上,大部分样品集中在碰撞前与碰撞后花岗岩区的分界处,以碰撞前为主；在Nb-Y图解上,样品落在火山弧-同碰撞花岗岩区；在Rb-(Y+Nb)图解上,样品点落在火山弧花岗岩区；在Rb-Hf-Ta图解上,样品全部落在弧系统岩石区.主体岩石中锆石Th/U值高,显示出岩浆锆石的特征,稀土元素总量高,重稀土元素富集明显,球粒陨石标准化图解曲线左倾,与岩浆锆石稀土元素配分曲线总体特征趋于一致.LA-ICP-MS锆石U-Pb定年表明其年龄为(253.5±7.9)Ma.杭嘎勒晚二叠世二长花岗岩为碰撞前火山弧花岗岩,研究区在晚二叠世时属于活动大陆边缘的火山弧.
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