宝石和宝石学杂志
寶石和寶石學雜誌
보석화보석학잡지
Journal of Gems & gemmology
2012年
2期
8-12
,共5页
韩文%洪汉烈%陈涛%殷科%吴钰%赵从华
韓文%洪漢烈%陳濤%慇科%吳鈺%趙從華
한문%홍한렬%진도%은과%오옥%조종화
“月尾紫”%寿山石%地开石%赤铁矿
“月尾紫”%壽山石%地開石%赤鐵礦
“월미자”%수산석%지개석%적철광
'Yueweizi'%larderite%dickite%hematite
针对采自福建寿山地区的寿山石“月尾紫”品种进行了光学显微镜、X射线粉末衍射、拉曼光谱和扫描电子显微镜等仪器的系统分析测试。结果显示,“月尾紫”呈显微微晶结构,主要矿物组成为地开石,基质中可见大量的紫红色矿物赤铁矿。赤铁矿呈浸染状分布,是致使“月尾紫”整体呈现紫色的原因。由于赤铁矿本身色调和富集程度不同,导致“月尾紫”的紫色调有深有浅,同时由于赤铁矿浸染分布于地开石颗粒间,使得“月尾紫”呈现不透明状。扫描电子显微镜下可见地开石颗粒主要呈假六方板状,棱角清晰,厚度均匀,呈叠瓦状、书册状排列,能谱测试结果显示扫描电子显微镜下微米级球状矿物颗粒为二氧化硅。
針對採自福建壽山地區的壽山石“月尾紫”品種進行瞭光學顯微鏡、X射線粉末衍射、拉曼光譜和掃描電子顯微鏡等儀器的繫統分析測試。結果顯示,“月尾紫”呈顯微微晶結構,主要礦物組成為地開石,基質中可見大量的紫紅色礦物赤鐵礦。赤鐵礦呈浸染狀分佈,是緻使“月尾紫”整體呈現紫色的原因。由于赤鐵礦本身色調和富集程度不同,導緻“月尾紫”的紫色調有深有淺,同時由于赤鐵礦浸染分佈于地開石顆粒間,使得“月尾紫”呈現不透明狀。掃描電子顯微鏡下可見地開石顆粒主要呈假六方闆狀,稜角清晰,厚度均勻,呈疊瓦狀、書冊狀排列,能譜測試結果顯示掃描電子顯微鏡下微米級毬狀礦物顆粒為二氧化硅。
침대채자복건수산지구적수산석“월미자”품충진행료광학현미경、X사선분말연사、랍만광보화소묘전자현미경등의기적계통분석측시。결과현시,“월미자”정현미미정결구,주요광물조성위지개석,기질중가견대량적자홍색광물적철광。적철광정침염상분포,시치사“월미자”정체정현자색적원인。유우적철광본신색조화부집정도불동,도치“월미자”적자색조유심유천,동시유우적철광침염분포우지개석과립간,사득“월미자”정현불투명상。소묘전자현미경하가견지개석과립주요정가륙방판상,릉각청석,후도균균,정첩와상、서책상배렬,능보측시결과현시소묘전자현미경하미미급구상광물과립위이양화규。
This paper investigates the mineralogical characteristics of "Yueweizi" (purple larderite) from Shoushan County, Fujian Province by using optical microscope, X-ray power diffraction (XRD), Raman spectroscopy and scanning electron microscope (with energy dispersive spectrome- ter, EDS). The results show that "Yueweizi" shows microcrystalline structure, that its main min- eral composition is dickite, and that there is a lot of purple-red hematite in the matrix. The purple colouration of "Yueweizi" is due tohematite. Because of the different amount of hematite, the purple colours have various saturations, and hematite also influences the transparency of the stone. The scanning electron microscope results show that the dickite particles appear as pseudohexagonal platy, have clear edges and almost the same thickness, and overlap with each other. The EDS test results show that the spherical particles are silicon dioxide.