内蒙古苏尼特左旗侵入岩谱系单位划分及岩浆演化特征

    HIERARCHY OF INTRUSIVE ROCK UNITS AND TECTONOMAGMATIC EVOLUTION IN THE SONID LEFT BANNER, INNER MONGOLIA

    • 摘要: 内蒙古苏尼特左旗南部地区岩浆活动强烈,古生代的深成侵入体大面积出露,大小岩体52个,面积约239km2。根据岩石谱系单位的划分原则及矿物成分和结构构造特征,划分为12个单元,归并为3个超单元。在对区内花岗岩的地质特征、岩石化学特征和稀土元素地球化学特征研究基础上,探讨了它们的演化和形成环境

       

      Abstract: Magmatic activity was strong in the southern part of the Sonid Left Banner, Inner Mongolia. Paleozoic plutons outcrop over large tracts. There are a total of 52 plutons of varying size, covering an area of about 239 km 2. In light of the principle for the hierarchical division, mineral composition and textures and structures, the plutonic rocks may be divided into 12 units, which are incorporated into three super units. On the basis of the geological, petrochemical and REE geochemical characteristics of granitoids in the study area, the author discusses their evolution and formation environment.

       

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