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大理北衙富碱斑岩侵入体的钾长石研究
Study on K-Feldspar of Baiya Alkali-Rich Prophyry in Dali District of Yunnan Province
【摘要】 探讨了北衙富碱斑岩侵入体之钾长石特征。其产出状态、结构状态、化学成分、形成温度等的研究表明,该钾长石具富Or之特点,其成分、结构等的变化在一定程度上反映了岩浆的演化特征,是岩浆演化的示踪矿物之一,可能是该区裂谷型碱性花岗岩的特征之一。
【Abstract】 This paper deals with the characteristics of kfeldspar in Baiya alkali一rich porphyry.The studyon its occurrence state,texture state,chemical compositions,forming temperatures etc。shows that thek-feldspar has higher or.The changes of its compositions,textures elc。can reflect magnatic evolution to①P.10some extent.It is one of the trace minerals of magnatic evolution, and may be one of the characters of therift-type alkali granitic rocks in this belt.
【关键词】 钾长石;
大理北衙;
富碱斑岩;
碱性花岗岩;
有序度;
【Key words】 K-Feldspar,Baiya,Dali,Alkali-Rich porphyry,Alkali granite; Order degree;
【Key words】 K-Feldspar,Baiya,Dali,Alkali-Rich porphyry,Alkali granite; Order degree;
- 【文献出处】 昆明工学院学报 , 编辑部邮箱 ,1994年01期
- 【分类号】P588.12
- 【被引频次】26
- 【下载频次】184