Permian magmatite distributes in Tarim Plate and surrounding area extensively,the complicated structure and lithic varity are always the discussing foucs in Beishan area of northeast of Tarim plate .
塔里木盆地及周边地区广泛分布着二叠纪岩浆岩,其中塔里木板块东北部的北山地区,由于构造复杂、岩性多样,一直为众学者争论的焦点。
参考来源 - 塔里木板块东北部二叠纪镁铁质—超镁铁质杂岩体成因·2,447,543篇论文数据，部分数据来源于NoteExpress
Wuyishan rare and precious metal ore belt is controlled by NE trend tectonic-magmatite belt.
武夷山稀有、贵金属矿带受ne向构造岩浆岩带控制。
The magmatite is characterized by the mantle-derived magma and the volcanic rocks occurring in orogenic belt.
岩浆岩具有幔源岩浆及造山带地区火山岩的特征。
Areas of experience and strong tectonic movement and almost every important crust tectonic movement, have corresponding magmatite, polycyclic magma activity.
区域经历了多阶段的强烈构造运动，而几乎每一次重要的地壳构造运动，都有相应的岩浆岩形成，具有多旋回岩浆活动特征。
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