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The garnets in the granitic gneisses from southern Dabie mountain were characterized by riching in Fe and Mn, and pooring in Mg, differing from the garnets in the UHP gneiss and eclogite, which relatively riching Mg. But the plagioclase in the granitic gneisses from the northern Dabie mountain was relative high Ca contenents, their An is 25.2-27.9, within the oligoclase field.
石榴石总体以贫Mg富Fe和富Mn为特征，明显不同于榴辉岩及高压片麻岩中石榴石相对富Mg的情况；而北大别英云闪长质片麻岩中斜长石的钙含量相对较高，An为25.2-27.9，位于奥长石范围内，角闪石中Mg的含量较高，具有壳幔混合源的特征。
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fasibitikite：钠闪锥辉花岗岩
钠闪正长岩 riebeckite syenite | 钠闪锥辉花岗岩 fasibitikite | 钠砷钙铀矿 sodium uranospinite
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messelite：水磷铁斜钙石
讯息杂波比 message-to-noise ratio | 水磷铁斜钙石 messelite | 暗色霞长岩,角闪辉霞石 mestigmerite