“海州式”磷矿床中磷灰石的矿物学研究
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Mineralogy of Apatites from Haizhou Type Phosphorite Deposits
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    摘要:

    “海州式”磷矿床中的磷灰石主要由变质改造再活化、混合岩化交代重结晶而成,有微 碳氟磷灰石、氟磷灰石两种,晶胞参数a0=9.3653-9.3819nm, co=6.8797-6.8936nm,晶体化 学式为(Ca5.ooFe0.02Sr0.01TR0.01)5.04 [(P2.99C0.04)3.03O12]F0.80,(Ca4.94Fe0.02mg0.02Sr0.01TR0.01)5.00 [(P2.90Ti0.02Si0.15)3.07O12]F0.77。本文还列出了磷灰石的红外吸收光谱,X射线衍射、化学成分和稀稀土元素含量等资料。

    Abstract:

    An integrated study of apatites from Haizhou type phosphorite deposits was madein such aspects as their mineral associations, chemical composition,REE analyses,inf-rared absorption spectra,and X-ray diffraction data. The results show that theseapatites were formed by metamorphic transformation-mobilization and migmatized meta-somatic recrystallization, and might be classified into two types:fluorapatite and fran-colite. Unit cell parameters a0=9.3653-9.3819nm,c0=6.8797 - 6.8936nm. Crystallo-chemical formulae (Ca5.00Fe0.02Sr0.01TR0.01)5.04[(P2.99C0.04)3.03O12]F0.08 and(Ca4.94Fe0.02 Mg0.02Sr0.01TR0.01)5.00 [(P2.90Ti0.02Si0.15)3.07)O12]F0.77). These data further demonstrate that the formationof Haizhou type phosphorite deposits is attributed mainly to deposition and metamor-phic transformation and next to migmatization-metasomatism.

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熊先孝,黄守英,1995,“海州式”磷矿床中磷灰石的矿物学研究[J].岩石矿物学杂志,14(3):271~280. Xiong Xianxiao, Huang Shouying,1995,Mineralogy of Apatites from Haizhou Type Phosphorite Deposits[J]. Acta Petrologica et Mineralogica,14(3):271~280.

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