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Calculated Nominal Ranges of Refractive Indices for the Amphiboles Found in the Rainy Creek Igneous Complex Near Libby, Montana

机译:在蒙大拿州利比附近的多雨小河火成岩复合体中发现的闪石的折光指数的标称标称范围

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The amphiboles occurring in the Rainy Creek Igneous Complex (RCC) near Libby, Montana, range in composition such that the following amphibole species have been identified: tremolite, winchite, richterite, magnesioriebeckite and magnesioarfvedsonite. The composition, optical and crystallographic values of only winchite and richterite have been determined. In an attempt to characterize the nominal (i.e. mean) refractive index for tremolite, magnesioriebeckite and magnesioarfvedsonite species, derivations of Gladstone-Dale constants specific to the RCC were attempted. It was not possible to obtain specific Gladstone-Dale constants using these data for the RCC amphiboles. Therefore, the Gladstone-Dale constants derived by Jaffe (1) for the alkali amphiboles were applied to the published electron probe microanalysis (EPMA) data from Meeker et al. (2) specific to tremolite and magnesioriebeckite, as well as the data from Sanchez et al. (3) for magnesioarfvedsonite. (Note: Dyar and Gunter [4], and references therein provide more information on amphibole nomenclature and correlations of refractive indices to mineral structures.) The range of nominal refractive indices for the tremolite, magnesioriebeckite and magnesioarfvedsonite are calculated as n=1.610 to 1.629, n=1.646 to 1.665 and n=1.641 to 1.652, respectively. The nominal range of refractive indices for the amphiboles occurring within the RCC is much smaller than the ranges for amphiboles under current International Mineralogical Association nomenclature for magnesioarfvedsonite and magnesioriebeckite and their solid solutions. Therefore, caution is required when using the optical properties of amphibole in asbestos determination at Libby.
机译:发生在蒙大拿州利比附近的雷尼河火成岩复合体(RCC)中的闪石组成范围使得可以确定以下闪闪石种:透闪石,Winchite,Richterite,Magnesioriebeckite和magnesioarfvedsonite。已确定仅白云石和Richterite的成分,光学和晶体学值。为了表征透闪石,镁硅锰矿和镁铝矾石种类的标称(即平均)折射率,尝试了特定于RCC的Gladstone-Dale常数的推导。使用这些RCC闪石的数据无法获得特定的Gladstone-Dale常数。因此,将Jaffe(1)推导的碱两性糖的Gladstone-Dale常数应用于Meeker等人发表的电子探针显微分析(EPMA)数据。 (2)特定于透闪石和菱镁矿,以及Sanchez等人的数据。 (3)镁铝矾石。 (注:Dyar和Gunter [4],及其中的参考文献提供了更多有关闪石命名法和折射率与矿物结构的相关性的信息。)透闪石,菱锰矿和镁铝矾石的标称折射率范围经计算为n = 1.610至1.629。 ,n = 1.646至1.665和n = 1.641至1.652。在RCC中发生的闪石的标称折射率范围远小于根据当前国际矿物学协会命名的镁闪石钠锰矿和镁硅锰矿及其固溶体的闪石的折射率范围。因此,在Libby的石棉测定中使用闪石的光学特性时,需要格外小心。

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