CNMNC多晶型和多聚体命名指南

IF 2.8 3区 地球科学 Q2 MINERALOGY
F. Hatert, S. Mills, M. Pasero, R. Miyawaki, F. Bosi
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引用次数: 2

摘要

摘要国际矿物学协会新矿物、命名和分类委员会(IMA–CNMNC)批准了多晶型和多聚体命名的新指南。可以区分几种情况。(i) 具有不同晶体系统的多晶型通过前缀cubo-(立方)、hexa-(六边形)、tetra-(四方)、trigo-(三角)、ortho-(斜方)、斜向(单斜)和anortho-(三斜)来区分。(ii)具有不同晶体系统但显示假对称性的多晶型应显示前缀“pseudo-”。(iii)具有相同晶体系统但不同空间群的多晶型通过前缀“para-”来区分。如果三个或三个以上的多晶型显示出相同的晶体系统但不同的空间群,则可以添加空间群符号作为后缀,尽管如果可能的话应该避免使用这种命名法。(iv)具有相同空间群的多面体通过前缀“para-”来区分。(v) 具有多晶型后缀但具有不同化学成分的矿物不能被视为真正的多晶型,因此我们建议使用前缀“meta-”,这表示一种接近但明显不同的化学成分。(vi)多体符号应作为后缀,表示结构中交替出现的模的数量和类型,如在högbomite超群中,或作为前缀,如在sartorite同源序列中。当作者决定使用结构前缀或后缀时,这些建议必须适用于未来的新矿产提案,但对历史和公认名称的修改必须通过CNMNC批准。为了与新的指导方针保持一致,现在修改了25个矿物名称:domeykite-β变为trigodomeyite;铁角石-(Y)-β变为斜铁角石(Y);铁角石-(Ce)-;铁角石-(Nd)-;冰VII变成立方冰;红柱石-β变为正长辉石;硫-β变为斜硫;mertieite II变为mertieite;mertieite-I变为假mertieite;铀烷-α变为铀烷;铀烷-β变为副铀烷;gersdorffite-P213变为gersdorfite;gersdorfite-Pa3变为paragersdorfite;gersdorffite-Pca21变为正交ersdorffite;倍他洛莫诺索夫岩变为副莫诺索夫岩;lammerite-β变为副氨铁矿;nováčekite-I变为Hydranováče ekite;nováčekite II变为novčikite;halloysite-7Å变为halloysite;halloysite-10Å变为氢halloysite;偏氧化铀-Ⅰ变为偏氧化铀;太肉豆蔻酸酯-I变为太肉豆蔻酯;二氧化铀变为二氧化铀;闪长岩IV变为四闪长岩;并且蓝帘石VI变为钠帘石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CNMNC guidelines for the nomenclature of polymorphs and polysomes
Abstract New guidelines for the nomenclature of polymorphs and polysomes have been approved by the the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA–CNMNC). Several cases can be distinguished. (i) Polymorphs with different crystal systems are distinguished by the prefixes cubo- (cubic), hexa- (hexagonal), tetra- (tetragonal), trigo- (trigonal), ortho- (orthorhombic), clino- (monoclinic) and anortho- (triclinic). (ii) Polymorphs with different crystal systems but showing a pseudosymmetry should show the prefix ‘pseudo-’. (iii) Polymorphs with the same crystal system but different space groups are distinguished by the prefix ‘para-’. If three or more polymorphs show the same crystal system but different space groups, the space group notation may be added as a suffix, though such a nomenclature should be avoided if possible. (iv) Polymorphs with the same space group are distinguished by the prefix ‘para-’. (v) Minerals with polymorph suffixes but with different chemical compositions cannot be considered as true polymorphs, so we recommend using the prefix ‘meta-’, which indicates a close but significantly different chemical composition. (vi) Polysomatic symbols should be placed as a suffix, which indicates the number and types of modules that alternate in the structure, such as in the högbomite supergroup, or as prefixes as in the sartorite homologous series. These recommendations have to be applied for future new mineral proposals, when the authors decide to use structural prefixes or suffixes, however modifications of historical and well-established names have to pass through the CNMNC for approval. In order to be consistent with the new guidelines, 25 mineral names are now modified: domeykite-β becomes trigodomeykite; fergusonite-(Y)-β becomes clinofergusonite-(Y); fergusonite-(Ce)-β becomes clinofergusonite-(Ce); fergusonite-(Nd)-β becomes clinofergusonite-(Nd); ice-VII becomes cubo-ice; roselite-β becomes anorthoroselite; sulphur-β becomes clinosulphur; mertieite-II becomes mertieite; mertieite-I becomes pseudomertieite; uranophane-α becomes uranophane; uranophane-β becomes parauranophane; gersdorffite-P213 becomes gersdorffite; gersdorffite-Pa3 becomes paragersdorffite; gersdorffite-Pca21 becomes orthogersdorffite; betalomonosovite becomes paralomonosovite; lammerite-β becomes paralammerite; nováčekite-I becomes hydronováčekite; nováčekite-II becomes nováčekite; halloysite-7Å becomes halloysite; halloysite-10Å becomes hydrohalloysite; metauranocircite-I becomes metauranocircite; taimyrite-I becomes taimyrite; uranocircite-II becomes uranocircite; andorite IV becomes quatrandorite; and andorite VI becomes senandorite.
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来源期刊
Mineralogical Magazine
Mineralogical Magazine 地学-矿物学
CiteScore
4.00
自引率
25.90%
发文量
104
审稿时长
6-12 weeks
期刊介绍: Mineralogical Magazine is an international journal of mineral sciences which covers the fields of mineralogy, crystallography, geochemistry, petrology, environmental geology and economic geology. The journal has been published continuously since the founding of the Mineralogical Society of Great Britain and Ireland in 1876 and is a leading journal in its field.
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