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八角手是最常用的宝石加工卡具,主要功能是实现宝石加工过程中分度的变化。分度的变化是通过八角手孔一边组合实现的,孔一边组合方式受孔位分布的影响。以最常用的64分度八角手为例,通过图解法和列表法,分析八角手孔位的分布原则,得出八角手的8个孔位应该分布在以正八边形模块对角线为基础,对圆形分度盘64等分,等分线与圆相交所形成的非八次对称点上。得出八角手的8个孔位是非八次对称的。并比较了3种不同形式孔位分布所形成的孔一边组合与分度的关系,得出孔位分布越规律、越集中,孔一边组合与分度的关系越简易、越直观,总结出三种孔一边组合方式与分度关系的计算公式,可以方便宝石加工人员在生产中变换分度操作的实用性,提高宝石加工的劳动生产力。 相似文献
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宝石加工工艺简介(一) 总被引:1,自引:0,他引:1
宝石加工工艺简介是陈兴汉高级工程师从事多年的宝石加工工艺研究与实践,并综合国内外有关资料总结编写的《宝石加工工艺学》一书的简要介绍。该书内容丰富,实用性强,具很高的参考价值。本刊将从刻面型宝石、素身型宝石、宝石项链的典型款式加工工艺方法及其常用设备类型和辅件材料等几个方面,陆续摘要刊登,供广大读者参考。 相似文献
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为了交流近年来我国宝石矿物学研究、生产和加工工艺方面取得的成果,促进我国天然宝石矿物的开发利用及人造宝石工业的发展,中国矿物岩石地球化学学会于6月21—24日在贵阳召开了全国宝石矿物学学术会议。出席会议的有中国科学院、高等院校、冶金部、地质矿产部、轻工业部、外贸部以及建材系统所属的67个单位93名代表. 会议共收到论文75篇。主要内容包括:(1)不同成因类型的宝石矿床成矿规律及找矿方向;(2)宝石矿物物理特性的测试;(3)人造宝石的生长工艺和生长机理研究;(4)宝玉石的鉴别及雕琢加工工艺。 相似文献
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新疆西南部帕米尔—西昆仑山区,近年来有许多新品种宝石发现和产出.其中,宝石级金刚石不断出土;优质红宝石、蓝宝石偶见于珠宝市场;优质方柱石(完全透明的和具有猫眼效应的)、榍石、透辉石等宝石已开始商品性生产.通过对上述宝石地质产出、宝石学特征、加工工艺特性试验的研究,认为这些宝石具有开发前景. 相似文献
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5 素身型宝石加工工艺5.1 素身型宝石主要款式及其特点 素身型宝石又称凸面型、弧面型、蛋面型、馒头型、大面型等。它是由简单的圆弧面组成,具有素雅大方艳美的特点。素身型宝石还具有用料种类多,石质不拘一格,产品用途广泛的特点,因而加工成的主要产品款式类型繁多,依其款式类型和特点具体划分如下。 相似文献
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6 宝石项链加工工艺6.1 宝石项链的款式类型及其加工工艺流程划分 宝石项链的款式类型很多,划分方案繁多,不同的方案各有其项链的名称。如按原料品种划分类型者,有水晶项链、玛瑙项链等;如按串链款式特点划分类型者,有平链、塔链、花链、复链等;若按项链珠粒形态划分类型者,有刻面型项链、圆珠型项链、随意型项链等。但是从加工工艺技术看,主要以按珠粒形态的分类较为恰当,因为不同形态的项珠粒加工工艺,对其原料 相似文献
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为了开发我国的宝石资源,更好地利用上海市场这一窗口,发挥上海在宝石地质、宝石鉴定、工艺和加工技术方面的优势,在上海市科学技术协会的关怀和支持下,经过一段时间的筹备工作,于1988年9月20日正式成立上海 相似文献
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深圳珠宝产业聚集区是中国内地最大的综合性珠宝首饰加工、制造与批发中心。近年来以万山工业区为中心逐渐形成翡翠批发市场,填补了深圳珠宝产业聚集区的空白。相对于广州、揭阳、平洲、四会等成熟翡翠市场来说,深圳翡翠市场仍属于一个新兴市场。对该翡翠市场进行了SWOT(即优势、劣势、机会与威胁)分析后认为,该市场的发展潜力巨大,但其竞争压力也十分严峻;同时,也为从业者正确认识该市场的环境态势、制定正确的经营策略、提高其竞争力、为深圳翡翠市场的健康、快速发展提供一定的指导。 相似文献
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The geochemical distribution of rubidium and strontium in the central granulite belt of Sri Lanka, where many of the gem deposits are found, was studied. The Rb-Sr ratios, particularly in the stream sediments, were found to be useful in delineating gem-bearing areas from the non gem-bearing or low potential areas. Among the main gem minerals that are mined at present are corundum, spinel, zircon and tourmaline. It was observed that higher Rb-Sr ratios correspond to high gem potential and, even within areas of good potential, barren areas could be delineated using these ratios. During pegmatite formation, Rb is enriched, and there is a marked depletion of Sr yielding a high Rb-Sr ratio. Pegmatites, granites and other magmatic bodies are associated with gem formation under granulite facies conditions and, when used in conjunction with geology, structure, and mineralogy, the Rb-Sr ratio could be used effectively to delineate target areas for further exploration. 相似文献
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应用光学显微镜及扫描电镜对双壳纲贝壳韧带结构色的研究表明,韧带具有非常美丽的结构色,可以做为宝石材料或收藏品.韧带结构色可能是由定向排列的纳米级文石及蛋白质纤维构成的光珊衍射引起的.韧带结构色的发现为宝石的颜色成因及光子带隙材料等研究提供了新的思路. 相似文献
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利用显微镜对重庆忠县翠屏山西晋时期崖墓出土的玛瑙珠、琥珀饰品和玻璃珠的表面痕迹进行了显微观察,对它们的加工工艺进行了分析和探讨。其中,玛瑙珠在粗磨过程中应使用了粒径较大、粒度不均匀的石英砂粒,导致玛瑙珠的外形不规整,表面多大而深的凹坑;琥珀饰品的钻孔外缘和表面存在较多应力裂纹,显示当时的玉匠对琥珀的加工尚不能克服琥珀性脆、怕热的缺点;玻璃珠至少可见铸造——切削成形、缠珠和直管切割3种制作工艺。这些饰品的特点反映了西晋时期平民社会所使用的饰品的面貌和工艺水平,为中国古代宝玉石和玻璃器的断代以及工艺研究提供了新的信息。 相似文献
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This classification of gem corundum (ruby and sapphire) deposits takes into consideration petrographic data, and the mode of genesis of the deposits. It is aimed at being practical and useful in the field, particularly for prospecting purposes.Deposits are classified into primary and secondary deposits. Primary deposits include igneous and metamorphic deposits. Igneous gem corundum deposits are rare and include sapphire-bearing syenites from Kenya. Emphasis is put on metamorphic deposits, that are subdivided into metamorphic s.s., metasomatic, and anatectic deposits. Many gem corundum deposits result from metasomatic processes. Small-scale metasomatism mostly involves desilication reactions between silico-aluminous rocks (pegmatites, gneisses, etc) and silica-poor rocks (ultramafites, meta-carbonates), and leads to the formation of limited-size deposits. Large-scale (diffuse) metasomatism is usually more difficult to characterize, and therefore is not separated from isochemical metamorphism in this classification. In metamorphic deposits, gem corundum results from transformation of an Al-rich and/or Si-poor protolith. Such deposits include ruby-bearing mafic granulites, ruby-bearing meta-limestones, and ruby/sapphire-bearing gneisses and granulites. An intermediate category includes anatectic deposits. Secondary deposits encompass sedimentary and volcanic (xenoclastic) occurrences. In sedimentary deposits, gem corundum occurs as clasts originating from other lithologies. In volcanic deposits, gem corundums are xenocrysts that have a range of origins.The proposed classification outlines geological environments favorable to the crystallization and distribution of gem corundum, thus facilitating prospecting and mining of this gemstone. 相似文献
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The most important source of yellow gem elbaite is the Canary mining area in the Lundazi District of eastern Zambia. The tourmaline has been mined since 1983 from both pegmatite and eluvial/alluvial deposits, in colors typically ranging from yellow-green to yellow to orange and brown; much of the orange-to-brown material is heated to attain a ‘golden’ or ‘canary’ yellow color. The elbaite is Mn-rich (up to 9.18 wt% MnO documented in the literature) and contains small amounts of Ti and little or no Fe. The distinctive composition of this tourmaline is probably the result of the early crystallization of abundant schorl from an unusual B-rich, Li-poor pegmatite melt, which depleted Fe while conserving Mn until the late-stage crystallization of gem pockets. The simple mineralogy of the pegmatite consists of feldspars, quartz, and tourmaline; the lack of micas, phosphates, or Li minerals, and the presence of very little garnet, allowed Mn to fractionate to high levels during pegmatite crystallization. The presence of abundant gem tourmaline in a Li-poor pegmatite is highly unusual. 相似文献
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本文在野外地质勘查及系统分析前人工作资料的基础上,对吉林省橄榄石宝石矿床区域分布及勘查开发现状进行归纳总结。吉林省橄榄石宝石矿主要分布在吉林省东部,已发现的橄榄石宝石矿床均赋存于新生界新近系上新统船底山组玄武岩中。严格受敦化-密山岩石圈断裂及其次级断裂控制。在找矿方向上应扩大已有矿区勘查范围,加大勘查力度及对省内船底山组玄武岩分布地区做重点勘查工作部署,力求在橄榄石宝石矿找矿方面取得更大的突破。同时对橄榄石宝石矿业发展远景进行探讨。 相似文献
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湖南金刚石内部不均一性特征研究 总被引:1,自引:0,他引:1
将湖南金刚石加工成片,利用宝石显微镜,偏光镜,阴极发光(CL)仪和傅里叶红外光谱(FTIR)仪对其内部显微特征进行了研究,发现金刚石的颜色深浅不一,内外颜色差异明显,呈带状,斑状分布;金刚石由生长中心至边缘,氮含量也有较大变化,中心与边缘最大相差约50倍,氮的富集类型由中心向边缘表现出B中心所占的比例越来越小,金刚石的类型也相应从I型→II型或I-aAB型→-I-aA型等,这些不均一性特征,反映金刚石在生长过程中环境条件发生了变化,以及生长期后可能受到了改造。 相似文献