Mineralogy of interior jewellery ammonites of the Samara region

D. A. Petrochenkov, E. Y. Baraboshkin
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引用次数: 1

Abstract

Background. Ammonite products are increasingly gaining in popularity. Ammonites are characterised by a variety of colour shades, shapes and sizes, making them suitable for manufacturing a wide range of souvenir and jewellery products. Russia enjoys significant resources of ammonites of interior and jewellery-ornamental quality; however, these materials remain insufficiently studied from the mineralogical point of view. This article presents the mineral composition and gemological characteristics of the Upper Jurassic interior jewellery ammonites of the Samara region for the first time.Aim. To describe the stratigraphic position and mineral composition of interior jewellery ammonites of the Samara region.Materials and methods. Late Jurassic ammonites (45 samples) were collected from a number of their main locations. The characteristic types of ammonites of interior-jewellery quality were distinguished and studied. Experiments included the determination of microhardness (25 determinations), density (12 determinations), luminescence features (10 samples), optical and petrographic analysis (5 thin sections), as well as the quantitative determination of mineral and chemical composition (3 samples), and electron probe studies (2 samples).Results. Ammonites are characterized by the presence of a mother-of-pearl layer with multi-coloured iridescence. The ammonites under study consist mainly of apatite (21—70 wt. %) and calcite (21—87 wt. %) along with quartz, aluminosilicates, gypsum, pyrite, zeolites, goethite, ilmenite and organic matter. The chambers of ammonite shells are made of phosphorite and calcite. The walls and partitions of shells have completely lost their original aragonite composition and consist of apatite and calcite with pyrite inclusions. The increased content of Sr (up to 0.17 wt. %) and Ba (up to 0.01 wt. %) are recorded as trace elements in ammonites. Calcite contains the following trace elements (wt. %): Mg — 0.17, Mn — 0.17, Fe — 1.14, Sr — 0.11, and Y — 0.17.Conclusion. The mineral and chemical (including microinclusions and trace elements) composition of interior-jewellery ammonites was established for the first time. The ammonites of the Samara region are of commercial interest as interior samples. Their shell fragments can be used in jewellery production. The ammonites under study can be collected along the coastal cliffs and beach area of the Volga river, thereby requiring no capital investments and producing no environmental pollution.
萨马拉地区室内珠宝菊石矿物学
背景。菊石产品越来越受欢迎。菊石具有多种颜色、形状和大小的特点,适合制造各种纪念品和珠宝产品。俄罗斯拥有丰富的室内和珠宝装饰品质的菊石资源;然而,从矿物学的角度来看,这些材料的研究还不够充分。本文首次介绍了萨马拉地区上侏罗统内部珠宝菊石的矿物组成和宝石学特征。描述萨马拉地区内部珠宝菊石的地层位置和矿物组成。材料和方法。晚侏罗世菊石(45个样本)从其主要位置采集。对室内珠宝品质的菊石特征类型进行了区分和研究。实验包括显微硬度测定(25个样品)、密度测定(12个样品)、发光特征测定(10个样品)、光学和岩石学分析(5个薄片)、矿物和化学成分定量测定(3个样品)和电子探针研究(2个样品)。菊石的特点是具有多色彩虹色的珍珠母层。所研究的菊石主要由磷灰石(21-70 wt. %)和方解石(21-87 wt. %)以及石英、铝硅酸盐、石膏、黄铁矿、沸石、针铁矿、钛铁矿和有机质组成。菊石壳的腔室由磷矿和方解石构成。贝壳的壁和隔板完全失去了原来的文石成分,由磷灰石、方解石和黄铁矿包裹体组成。其中Sr (0.17 wt. %)和Ba (0.01 wt. %)的含量增加,是菊石中的微量元素。方解石含有以下微量元素(wt. %): Mg - 0.17, Mn - 0.17, Fe - 1.14, Sr - 0.11, Y - 0.17。首次确定了首饰内菊石的矿物和化学组成(包括微包裹体和微量元素)。萨马拉地区的菊石作为内部样品具有商业价值。它们的贝壳碎片可以用来制作珠宝。所研究的菊石可以在伏尔加河沿岸的悬崖和海滩地区采集,不需要任何资本投资,也不会产生环境污染。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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