山东枣庄沙沟环状偏碱性杂岩体中磷灰石特征及地质意义
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Apatite from the Shagou Ringed Subalkalic Complex in Zaozhuang,Shandong Province-Its Characteristics and Geological Significance
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    摘要:

    枣庄偏碱性杂岩体侵位于泰山群片麻岩中,同位素年龄测定为101—133百万年。本文主要讨论了磷灰石特征与成因的关系。研究了磷灰石稀土元素配分、x射线衍射、晶胞参数、红外光谱等特征,探讨了磷灰石形成温度,磷的富集作用与物理化学条件以及磷矿床的成因类型。

    Abstract:

    Emplaced in gneiss of Taishan Group, the Zaozhuang subalkalic complexhas an isotopic age of 101--133Ma. The present paper deals Inainly with the relationship between typomorphiccharacteristics of apatite and its origin, makes an examination on such experi-mental data of. apatite as REE distribution, X-ray diffraction, crystal unitparameters and infrared spectra, and conducts a tentative investigation into theformation temperature of apatite, the concentration of P2O5, the physical-che-mical condition for ore formation and the genetic type of apatite deposit.

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夏学惠,刘昌涛, 1987. 山东枣庄沙沟环状偏碱性杂岩体中磷灰石特征及地质意义[J]. 岩石矿物学杂志, 6(4):357~363.
Xia Xuehui, Liu Changtao Geological Institute, Ministry of Chemical Industry, et al, 1987. Apatite from the Shagou Ringed Subalkalic Complex in Zaozhuang,Shandong Province-Its Characteristics and Geological Significance[J]. Acta Petrologica et Mineralogica, 6(4): 357~363.

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