香花岭地区在湖南省临武县城以北约20km处,位于南岭东西向稀有金属成矿带的中段。在构造上,本区 为一背斜弯隆,其中心由寒武系浅海相复理石建造组成,
香花岭碱长花岗岩为一复式岩体。
Xianghualing alkali-feldspathic granite is a composite rock mass.
氧化物构造环境判别图解及区域构造演化背景反映香花岭岩体形成于后造山构造环境。
Multiple oxide-diagrams for discrimination of structural environment and regional tectonic evolution background indicate that the rocks were formed in a post-orogenic extension environment.
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