首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Avdoninite,K2Cu5Cl8(OH)4 centre dot H2O,a New Mineral Species from Volcanic Exhalations and the Technogenic Zone at Volcanic-Hosted Massive Sulfide Deposits
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Avdoninite,K2Cu5Cl8(OH)4 centre dot H2O,a New Mineral Species from Volcanic Exhalations and the Technogenic Zone at Volcanic-Hosted Massive Sulfide Deposits

机译:Avdoninite,K2Cu5Cl8(OH)4中心点H2O,来自火山呼出和火山岩质大块硫化物矿床成矿带的新矿物物种

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Avdoninite,a new mineral species,has been found together with euchlorite,paratacamite,atacam-ite,belloite,and langbeinite hosted in exhalation sediments of the Yadovitaya fumarole in the Second Cinder Cone at the Northern Breach of the Great Fissure Tolbachik Eruption,Tolbachik volcano,Kamchatka Peninsula,Russia.Avdoninite occurs as imperfect,short prismatic and thick tabular crystals up to 0.2 mm long,with (001) and (100) forms,crystal aggregates,and pseudomorphs (together with atacamite) after melanothallite observed.The new mineral is brittle,with the Mohs hardness 3 (for aggregates).Density is 3.03 g/cm3 (meas.) and 3.066 g/cm3 (calc).Avdoninite is biaxial and optically neutral,with alpha = 1.669,beta = 1.688,gamma= 1.707,2V = -90°.Dispersion is not observed.Optical orientation:Y= c,X = bl Pleochroism is absent.The infrared spectrum suggests the presence of water molecules in avdoninite.Electron microprobe chemical analysis has given (wt %) K2O 11.94 (±0.4),CuO 51.43 (±0.7),Cl 37.07 (±0.6),H2O (determined by the Penfield method) 6.9,-0=C12 -8.37,total 98.97.The empirical formula is K1.96Cu5.00Cl8.09(OH)3.87 centre dot 1.03H2O.Avdoninite is mono-clinic,space group P2/m,P2,or Pm;a = 24.34(2) A,' b = 5.878(4) A,c = 11.626(5) A,beta = 93.3(1)°,V = 1660.6(20) A3,Z = 4.The compatibility index is good:1 - K_pK_c = 0.056 for D_(calc) and 0.044 for Z)_(meas).The strongest lines in the X-ray powder diffraction pattern (d,A (I,%) (hkl)) are 11.63(100)(001),5.88(20)(010),5.80(27)(002),5.73(17)(102),2.518(19)(214),2.321(17)(005).Avdoninite is identical to a technogenic analogue previously described from the Blyava volcanic-hosted massive sulfide deposit,Orenburg oblast,Russia.The new mineral is named after Vladimir Nikolaevich Avdonin (born 1925),a senior researcher of the Ural Geological Museum of the Ural State Mining University.The type material of avdoninite from Kamchatka is deposited in the Mineralogical Museum of the Department of Mineralogy,St.Petersburg State University,St.Petersburg,Russia.The registration number is 19175.
机译:在大裂隙托尔巴奇克火山喷发带北部断裂的第二煤渣锥中,Yadovitaya fumarole的呼出沉积物中发现了一种新的矿物种,一种名为Avdoninite的矿物,其中还包含了绿藻石,顺滑石,atacamite,贝洛石和langbeinite。 ,Kamchatka半岛,俄罗斯。Avdoninite是不完美的,短的棱柱形且厚的片状晶体,长达0.2 mm长,具有(001)和(100)形式,晶体聚集,并且在观察到黑硅藻土后产生假晶形(连同滑石)。新矿物脆性,莫氏硬度3(对于骨料)。密度为3.03 g / cm3(平均)和3.066 g / cm3(计算).Avdoninite是双轴且光学中性的,α= 1.669,β= 1.688,γ= 1.707,2V = -90°。未观察到分散。光学方向:Y = c,X = bl不存在多发色性。红外光谱表明在钠云母中存在水分子。电子探针化学分析得出(wt%)K2O 11.94(±0.4),CuO 51.43(±0.7),Cl 37.0 7(±0.6),H2O(通过Penfield方法测定)6.9,-0 = C12 -8.37,总计98.97。经验公式为K1.96Cu5.00Cl8.09(OH)3.87中心点1.03H2O。临床,空间组P2 / m,P2或Pm; a = 24.34(2)A,'b = 5.878(4)A,c = 11.626(5)A,beta = 93.3(1)°,V = 1660.6( 20)A3,Z = 4相容性指数良好:D-(calc)的K-pK_c = 0.056,Z)_(meas)的K = 0.044.X射线粉末衍射图(d,A( I,%)(hkl))是11.63(100)(001),5.88(20)(010),5.80(27)(002),5.73(17)(102),2.518(19)(214),2.321 (17)(005).Avdoninite与先前在俄罗斯奥伦堡州Blyava火山携带的块状硫化物矿床中描述的技术类似物。新矿物以弗拉基米尔·尼古拉耶维奇·阿夫多宁(Vladimir Nikolaevich Avdonin,出生于1925年)命名。乌拉尔州立矿业大学的乌拉尔地质博物馆。来自堪察加的钠钙矾的典型材料存放在圣彼得堡国立大学矿物学系矿物学博物馆俄罗斯圣彼得堡。注册号为19175。

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