宝石和宝石学杂志
寶石和寶石學雜誌
보석화보석학잡지
Journal of Gems & gemmology
2011年
4期
19-25
,共7页
墨绿色钠长石玉%化学成分%镁钠铁闪石%有序度%形成温度
墨綠色鈉長石玉%化學成分%鎂鈉鐵閃石%有序度%形成溫度
묵록색납장석옥%화학성분%미납철섬석%유서도%형성온도
dark-green albite jade%chemical composition%magnesioarfvedsonite%degree of order%formation temperature
以墨绿色钠长石玉样品为研究对象,采用常规的宝石学测试、偏光显微镜、电子探针、X射线粉末衍射等分析方法,从宝石学特征、矿物组成、结构特征、有序度等方面,对该钠长石玉进行了较全面的研究。结果表明,墨绿色钠长石玉的折射率为1.53(点测),密度约为2.64g/cm^3;其薄片中矿物晶体的形态主要呈半自形-他形粒状、短柱状和纤维状,结构主要有糜棱结构和纤维粒状变晶结构,主要矿物组成为钠长石和角闪石。电子探针的化学成分分析显示,样品中钠长石的An值小于0.006,说明钠长石的成分很纯;所含的角闪石种类主要为镁钠铁闪石。由X射线粉末衍射峰数据计算出钠长石的结构有序度极接近于1,其为完全有序的低钠长石,形成温度低于300℃。本文填补了钠长石玉研究中的一些空缺,为钠长石玉的系统性和综合性研究提供一些有意义的理论成果。
以墨綠色鈉長石玉樣品為研究對象,採用常規的寶石學測試、偏光顯微鏡、電子探針、X射線粉末衍射等分析方法,從寶石學特徵、礦物組成、結構特徵、有序度等方麵,對該鈉長石玉進行瞭較全麵的研究。結果錶明,墨綠色鈉長石玉的摺射率為1.53(點測),密度約為2.64g/cm^3;其薄片中礦物晶體的形態主要呈半自形-他形粒狀、短柱狀和纖維狀,結構主要有糜稜結構和纖維粒狀變晶結構,主要礦物組成為鈉長石和角閃石。電子探針的化學成分分析顯示,樣品中鈉長石的An值小于0.006,說明鈉長石的成分很純;所含的角閃石種類主要為鎂鈉鐵閃石。由X射線粉末衍射峰數據計算齣鈉長石的結構有序度極接近于1,其為完全有序的低鈉長石,形成溫度低于300℃。本文填補瞭鈉長石玉研究中的一些空缺,為鈉長石玉的繫統性和綜閤性研究提供一些有意義的理論成果。
이묵록색납장석옥양품위연구대상,채용상규적보석학측시、편광현미경、전자탐침、X사선분말연사등분석방법,종보석학특정、광물조성、결구특정、유서도등방면,대해납장석옥진행료교전면적연구。결과표명,묵록색납장석옥적절사솔위1.53(점측),밀도약위2.64g/cm^3;기박편중광물정체적형태주요정반자형-타형립상、단주상화섬유상,결구주요유미릉결구화섬유립상변정결구,주요광물조성위납장석화각섬석。전자탐침적화학성분분석현시,양품중납장석적An치소우0.006,설명납장석적성분흔순;소함적각섬석충류주요위미납철섬석。유X사선분말연사봉수거계산출납장석적결구유서도겁접근우1,기위완전유서적저납장석,형성온도저우300℃。본문전보료납장석옥연구중적일사공결,위납장석옥적계통성화종합성연구제공일사유의의적이론성과。
The gemmological characteristics,mineral components,texture feature and degree of order of the dark-green albite jade are systematically studied by using many kinds of analytical methods,such as conventional gemmological methods,polarizing microscope,electron microprobe and X-ray powder diffraction.The results show that the refractive index of the dark-green albite jade is about 1.53 with density of 2.64 g/cm3.In the petrographic thin sections,the mineral crystals are mainly hypidiomorphic to xenomorphic granular,short prismatic and fibrous.There are two major kinds of texure,mylonitic texture and fibrous granular crystalloblastic texture.The main mineral components are albite and amphibole.The results of chemical compositions of samples by using electron microprobe are that the values of An of albite is less than 0.006,which suggests that the albite ingredient is very pure.The major amphibole type is magnesioarfvedsonite.Based on the X-ray powder diffraction data,the degree of order of albite structure has been calculated,which is very close to 1.It is completely ordered low albite.The formation temperature is lower than 300℃.The present paper makes up some deficiencies in the research on albite jade and provides some meaningful theoretical achievements for the further systematic and comprehensive research on it.