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Feldspars (including albite and K-feldspar) and amblygonite are the main reserves of the whole-rock phosphorus in the Yashan topaz-lepidolite granite, and the contribution of feldspars to whole-rock phosphorus is related with the crystallization of amblygonite.
长石及磷锂铝石是雅山黄玉锂云母花岗岩中磷的主要贮体，磷锂铝石的出现与否直接影响了长石的磷含量及其对全岩磷的贡献率。
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If without amblygonite in crystallization assemblage, the feldspars contribute above 70% of whole-rock phosphorus, otherwise the amblygonite is the main reserves of whole-rock phosphorus and the feldspars are the subordinate.
无磷锂铝石晶出时，长石磷对全岩磷的贡献率达70％以上；当具磷锂铝石晶出时，磷锂铝石为全岩磷的主要贡献，长石降为次要地位。
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Anorthite and albite are important calcium-containing feldspars.
钙长石与钠长石是重要的含钙长石。
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"It is the most abundant metallic element in Earth's crust, chiefly in bauxite, feldspars, mica s, clay minerals, and laterite. It also occurs in gemstones, such as topaz, garnet, and chrysoberyl; emery, corundum, ruby, and sapphire are crystalline aluminum oxide."
为地壳中丰度最高的金属元素，多存在于铝土矿、长石、云母、黏土等矿物和砖红壤中，也存在于宝石之内，如黄宝石、红宝石及金绿宝石；而刚玉金刚砂、深红宝石及蓝宝石则为晶透的氧化铝。
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"It is the most abundant metallic element in Earth's crust, chiefly in bauxite, feldspars, micas, clay minerals, and laterite. It also occurs in gemstones, such as topaz, garnet, and chrysoberyl; emery, corundum, ruby, and sapphire are crystalline aluminum oxide ."
为地壳中丰度最高的金属元素，多存在于铝土矿、长石、云母、黏土等矿物和砖红壤中，也存在于宝石之内，如黄宝石、红宝石及金绿宝石；而刚玉金刚砂、深红宝石及蓝宝石则为晶透的氧化铝。
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monzodiorite：二长闪长岩
6区和 7 区- 这两个区岩石的基本名称分别为碱长正长岩(alkali-feldspars yenite)和正长岩9区- 本区有两个基本名称,即二长闪长岩(monzodiorite)和二长辉长岩(monzogabbro),可根据为二长闪长岩;如斜长石An大于50%并主要含辉石时,
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monzogabbro：二长辉长岩
6区和 7 区- 这两个区岩石的基本名称分别为碱长正长岩(alkali-feldspars yenite)和正长岩9区- 本区有两个基本名称,即二长闪长岩(monzodiorite)和二长辉长岩(monzogabbro),可根据为二长闪长岩;如斜长石An大于50%并主要含辉石时,