镁铝榴石是石榴石中的一种,它是含镁铝的石榴子石,以其结构透明而用为宝石。其颜色变化于淡褐红色至淡紫红色之间。化学成分为Mg3Al2(SiO4)3,其中常见少量的Fe、Mn代换Mg。
锆石、镁铝榴石则质量较好,研究其矿物组合对矿床的综合开发具有应用的意义。
Zircon and almandine possess high quality. Studying the mineral is plays an important for comprehensively developing and exploiting the deposit.
石榴石的种类包括(铁铝榴石、镁铝榴石、镁铁榴石、锰铝榴石、钙铁榴石、钙铬榴石)。
The variety of garnet includes almandine, pyrope, magnesium-iron garnet, manganese-aluminum garnet, andradite and calcium-chromium garnet.
镁铝榴石形成于滇东南晚第三纪岩简状的玄武质次火山角砾岩中,角砾岩成分复杂,其中包含有镁铝榴石和铬透辉石等可作宝石材料利用的角砾和晶屑。
The rubbles and crpetals of prrope and chrome-diopsidewhich can be used as gem materials are found in the breccias whose component is very complex.
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