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Nomenclature of the triphylite group of minerals
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Abstract. In this paper we present a Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA-CNMNC)-accepted scheme for the
classification and nomenclature of the triphylite group of minerals. The
general formula of those minerals is M1M2TO4, where M1 and M2 refer to
cations in an octahedral coordination: M1 = □, Na, Li; M2 = Mn2+,
Fe2+, Mg, Fe3+, Mn3+, and T to tetrahedrally coordinated
P5+ cations. The group contains the Li-bearing phosphates triphylite
[LiFe2+(PO4)] and lithiophilite [LiMn2+(PO4)] and their
oxidation products heterosite [Fe3+(PO4)] and purpurite
[Mn3+(PO4)], as well as the Na-bearing phosphates natrophilite
[NaMn2+(PO4)] and karenwebberite [NaFe2+(PO4)]. The
Li–Mg-bearing phosphate simferite has been redefined as LiMg(PO4).
Ferrisicklerite and sicklerite correspond to intermediate phases in the
triphylite–heterosite and lithiophilite–purpurite solid solutions;
consequently, according to the CNMNC dominant-constituent rule, they are
discredited. A new mineral oxidation sequence is defined, which considers
the different oxidation capacity of iron and manganese, and therefore
replaces the traditional Quensel–Mason sequence. The formula calculation
procedure for Li-bearing species, based on electron microprobe analyses and
single-crystal X-ray diffraction data, is also described.
Title: Nomenclature of the triphylite group of minerals
Description:
Abstract.
In this paper we present a Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA-CNMNC)-accepted scheme for the
classification and nomenclature of the triphylite group of minerals.
The
general formula of those minerals is M1M2TO4, where M1 and M2 refer to
cations in an octahedral coordination: M1 = □, Na, Li; M2 = Mn2+,
Fe2+, Mg, Fe3+, Mn3+, and T to tetrahedrally coordinated
P5+ cations.
The group contains the Li-bearing phosphates triphylite
[LiFe2+(PO4)] and lithiophilite [LiMn2+(PO4)] and their
oxidation products heterosite [Fe3+(PO4)] and purpurite
[Mn3+(PO4)], as well as the Na-bearing phosphates natrophilite
[NaMn2+(PO4)] and karenwebberite [NaFe2+(PO4)].
The
Li–Mg-bearing phosphate simferite has been redefined as LiMg(PO4).
Ferrisicklerite and sicklerite correspond to intermediate phases in the
triphylite–heterosite and lithiophilite–purpurite solid solutions;
consequently, according to the CNMNC dominant-constituent rule, they are
discredited.
A new mineral oxidation sequence is defined, which considers
the different oxidation capacity of iron and manganese, and therefore
replaces the traditional Quensel–Mason sequence.
The formula calculation
procedure for Li-bearing species, based on electron microprobe analyses and
single-crystal X-ray diffraction data, is also described.
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