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黑青和田玉宝石矿物学及地球化学特征研究OA北大核心CSTPCD

Gem mineralogical and geochemical characteristics of the black cyan nephrite

中文摘要英文摘要

近年国内市场出现了一种含有黄铁矿的黑青色玉石,主要产自新疆,属于和田玉中的稀少品种.本文利用常规宝石学仪器、偏光显微镜、红外光谱、拉曼光谱、X射线粉晶衍射(XRD)、电子探针(EPMA)、激光电感耦合等离子质谱(LA-ICP-MS)以及同位素质谱仪(MC-ICP-MS)对7块黑青和田玉样品的宝石矿物学和地球化学特征进行了系统分析,结果显示,样品颜色为墨绿-黑色,折射率点测1.61,相对密度3.08~3.17,摩氏硬度6.0~6.5,主要组成矿物为透闪石,次要矿物以黄铁矿为主,同时还含有少量绿泥石、绿帘石、榍石、锆石、石墨等,具有典型的纤维交织状结构;红外与拉曼光谱特征峰显示与和田玉标准谱峰一致;样品中透闪石的主要化学成分为SiO2、MgO、CaO和FeO,Mg/(Mg+Fe2+)值显示部分透闪石已过渡为阳起石;根据微量元素Cr-Ni投图判别样品为白云石大理岩型成因,稀土元素含量较少,呈左倾模式;推测成矿热液主要为岩浆水,含少量变质水;样品中黄铁矿Co/Ni>1且含少量As、Se、Cu、Zn、Pb等元素,δ34S介于8.87‰~20.92‰之间,推断为岩浆热液成因且硫来源于岩浆与地层硫的混合.

In recent years,a kind of black cyan nephrite containing pyrite has appeared in the domestic market.It is mainly produced in Xinjiang and belongs to a relatively rare nephrite variety,which has mining and utilization value.This article systematically analyzed the mineralogical and geochemical characteristics of seven samples using conventional gemological instruments,polarized light microscopy,infrared spectroscopy,Raman spectroscopy,X-ray powder diffraction(XRD),electron probe(EPMA)laser inductively coupled plasma mass spectrometry(LA-ICP-MS),and isotope mass spectrometer(MC-ICP-MS).The results show that the color of black cyan neph-rite is dark green to black,the refractive index is 1.61,the relative density is 3.08~3.17,and the Mohs hardness is 6.0~6.5.The main component mineral is tremolite,the secondary mineral is mainly pyrite,and a small amount of chlorite,epidote,sphene,zircon,and graphite are also contained,with a typical fiber interlaced struc-ture;The characteristic peaks of infrared and Raman spectra are consistent with the standard peaks of nephrite;The main chemical components of the sample are SiO2,MgO,CaO and FeO.The Mg/(Mg+Fe2+)value indicates that some tremolite has transitioned to actinolite.Based on the trace element Cr-Ni mapping,the sample is identified as a dolomite marble type genesis,while the content of rare earth elements is relatively low,in a left leaning mode,The ore-forming hydrothermal fluid is mainly magmatic water,containing a small amount of metamorphic water.The sample contains pyrite with Co/Ni>1 and small amounts of As,Se,Cu,Zn and Pb,δ34Sranges from 8.87%o to 20.92%o,suggesting that it is of magmatic-hydrothermal origin and the source of sulfur is a mixture of magma and formation sulfur.

付玉蕾;史淼;曹沁元;马世玉

河北地质大学,河北石家庄 050031||中国地质调查局 自然资源实物地质资料中心,河北三河 065201河北地质大学,河北石家庄 050031||河北省岩石矿物材料绿色开发重点实验室,河北石家庄 050031||硅酸盐固废资源化利用河北省工程研究中心,河北石家庄 050031河北地质大学,河北石家庄 050031

地质学

黑青和田玉;黄铁矿;宝石矿物学;氢-氧-硫同位素

black cyan nephrite;pyrite;gemology and mineralogy;hydrogen-oxygen-sulfur isotope

《岩石矿物学杂志》 2024 (003)

630-642 / 13

National Natural Science Foundation of China(42002156);Natural Science Foundation of Hebei Provincial(D2021403015);Science and Technology Project of Hebei Education Department(QN2021027);National Pre-research Project of Hebei Geology University(KY2024YB01) 国家自然科学基金项目(42002156);河北省自然科学基金项目(D2021403015);河北省高等学校科学技术研究项目(QN2021027);河北地质大学国家预研项目(KY2024YB01)

10.20086/j.cnki.yskw.2024.0311

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