Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1482.05
Yurichev А.N., Che-Ani A.I, Korbovyak E.V.
{"title":"Platinum group minerals from chromitites of Kempirsai ultramafic massif (the South Urals): new data","authors":"Yurichev А.N., Che-Ani A.I, Korbovyak E.V.","doi":"10.30695/zrmo/2019.1482.05","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1482.05","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69567232","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1483.08
Slukovskii Z.I., Dauvalter V.A.
{"title":"Morphology and composition of technogenic particles in bottom sediments of the lake Nudyavr, Murmansk Region","authors":"Slukovskii Z.I., Dauvalter V.A.","doi":"10.30695/zrmo/2019.1483.08","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1483.08","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69567241","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1483.01
Vasilenko V.B., Zinchuk N.N., Kuznetsova L.G.
{"title":"Conjugation of chemical compositions of rocks and accessory minerals in kimberlites","authors":"Vasilenko V.B., Zinchuk N.N., Kuznetsova L.G.","doi":"10.30695/zrmo/2019.1483.01","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1483.01","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"39 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69567406","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1485.07
Rudashevsky N.S., Rudashevsky V.N.
{"title":"New data on malanite and cuprorhodsite from chromitites of the Bushveld Complex, South Africa","authors":"Rudashevsky N.S., Rudashevsky V.N.","doi":"10.30695/zrmo/2019.1485.07","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1485.07","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69574312","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1486.03
Petrovskiy M.N.
{"title":"Rare-earth minerals of carbonate veins in the Soustov massif (Kola Peninsula) as an the indicator of its ore specialization","authors":"Petrovskiy M.N.","doi":"10.30695/zrmo/2019.1486.03","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1486.03","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69574326","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1485.01
Gulbin Y.L., Mikhalsky E.V.
{"title":"Modeling of mineral parageneses and thermobarometry of metavolcanic rocks of the Ruker Group in the Southern Prince Charles Mountains, East Antarctica","authors":"Gulbin Y.L., Mikhalsky E.V.","doi":"10.30695/zrmo/2019.1485.01","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1485.01","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69574206","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/ZRMO/2019.1483.02
A. Kasatkin, Касаткин Анатолий Витальевич, S. Britvin, Бритвин Сергей Николаевич, N. Chukanov, Чуканов Никита Владимирович, R. Škoda, Шкода Радек, A. Agakhanov, Агаханов Атали Акмурадович, D. Belakovskiy, Белаковский Дмитрий Ильич
Belogubite, ideally CuZn(SO 4 ) 2 ·10H 2 O, has been found in the supergene zone uncovered by the open pit at the Gayskoe massive sulfide Zn-Cu deposit (Orenburgskaya region, the South Urals, Russia). It is associated with dietrichite and may contain relics of quartz. Belogubite forms aggregates of blue grains up to 1 mm in size. The mineral is transparent with vitreous luster and white streak. Its color varies from pale equant to light blue. Cleavage and parting were not observed. The new mineral is brittle and has Mohsʼ hardness ca . 2½. Its density measured by floatation in bromoform+ethanol is 2.27(2) g/cm –3 , its calculated density is 2.249 g/cm –3 . Belogubite is biaxial (–), α = 1.512(2), β = 1.525(2), γ = 1.531(2); 2 V (meas.) = 70(10)°, 2 V (calc.) = 67.9°. Dispersion is noticeable, r < v . The mineral is nonpleochroic. Chemical composition of the holotype sample is (wt %, electron microprobe data, H 2 O determined by thermogravimetry): MgO 1.12, MnO 0.10, FeO 3.15, CuO 8.98, ZnO 18.02, SO 3 32.49, H 2 O 36.75, total 100.61. Its empirical formula calculated on the basis of 18 O apfu is: (Cu 0.55 Zn0 .45 ) Σ1.00 (Zn 0.64 Fe 0.22 Mg 0.14 Mn 0.01 ) Σ1.01 S 1.99 O 7.98 ·10.02H 2 O. The structure was solved by direct methods and refined on the basis of 1797 independent reflections to R = 0.016. Belogubite is triclinic, P 1 . Unit cell parameters are: a = 6.2548(1), b = 10.6112(2), c = 6.0439(1) A, α = 82.587(1), β = 109.625(1), γ = 104.848(1)°, V = 364.81(1) A 3 , Z = 1. The strongest reflections of the powder XRD pattern are [ d obs , A ( I ) ( hkl )]: 5.73 (35) (100), 5.576 (47) (–110), 4.873 (100) (–111), 3.907 (31) (021), 3.719 (45) (0 –21), 3.229 (27) (111), 2.915 (25) (–221), 2.684 (26) (130). Belogubite is a new, CuZn-ordered member of the chalcanthite group having M 1 cationic site preferentially occupied by Cu whereas M 2 site is dominated by Zn with subordinate substitution of Fe 2+ and Mg. The mineral is named in honor of Elena Vitalievna Belogub (born 1963), major researcher of the Institute of Mineralogy of the Urals Branch of Russian Academy of Sciences, Miass, Chelyabinsk Oblast, Russia, a well-known expert in the mineralogy of volcanic-hosted massive sulfide copper deposits of South Urals.
在俄罗斯南乌拉尔Orenburgskaya地区Gayskoe块状硫化物锌铜矿露天矿裸露的表生带中发现了别氏石英，理想值为CuZn(so4) 2·10h2o。它与二辉石伴生，可能含有石英遗迹。贝洛格石形成大小达1毫米的蓝色颗粒聚集体。该矿物透明，具有玻璃光泽和白色条纹。它的颜色从淡蓝色到浅蓝色不等。未观察到解理和分型。这种新矿物易碎，具有莫氏硬度。2½。经溴甲烷+乙醇浮选测定其密度为2.27(2)g/cm -3，计算密度为2.249 g/cm -3。Belogubite双轴(-),α= 1.512(2),β= 1.525(2),γ= 1.531 (2);2v(平均值)= 70(10)°，2v (calc) = 67.9°。色散明显，r < v。这种矿物是非多色性的。样品的化学成分为(wt %，电子探针数据，h2o由热重法测定):MgO 1.12, MnO 0.10, FeO 3.15, CuO 8.98, ZnO 18.02, so3 32.49, h2o 36.75, total 100.61。基于18 O apfu计算出的经验公式为:(Cu 0.55 zn0.45) Σ1.00 (Zn 0.64 Fe 0.22 Mg 0.14 Mn 0.01) Σ1.01 S 1.99 O 7.98·10.02 h2o。该结构采用直接法求解，并根据1797次独立反射修正为R = 0.016。贝洛格石是三斜的，p1。晶胞参数:= 6.2548 (1),b = 10.6112 (2), c = 6.0439(1),α= 82.587(1),β= 109.625(1),γ= 104.848(1)°,V = 364.81 (1) 3, Z = 1。粉末XRD谱图的最强反射为[d obs, A (I) (hkl)]: 5.73(35)(100)、5.576(47)(-110)、4.873(100)(-111)、3.907(31)(021)、3.719(45)(0 -21)、3.229(27)(111)、2.915(25)(-221)、2.684(26)(130)。辉绿石是一种新的、cuzn有序的辉绿石群成员，其m1阳离子位优先被Cu占据，而m2阳离子位以Zn为主，次要取代fe2 +和Mg。该矿物的命名是为了纪念Elena Vitalievna Belogub(生于1963年)，她是俄罗斯车里雅宾斯克州米斯市俄罗斯科学院乌拉尔分院矿物学研究所的主要研究员，也是南乌拉尔火山带块状硫化物铜矿矿物学方面的知名专家。
{"title":"Belogubite, a new mineral of the chalcanthite group from the Gayskoe deposit, South Urals, Russia","authors":"A. Kasatkin, Касаткин Анатолий Витальевич, S. Britvin, Бритвин Сергей Николаевич, N. Chukanov, Чуканов Никита Владимирович, R. Škoda, Шкода Радек, A. Agakhanov, Агаханов Атали Акмурадович, D. Belakovskiy, Белаковский Дмитрий Ильич","doi":"10.30695/ZRMO/2019.1483.02","DOIUrl":"https://doi.org/10.30695/ZRMO/2019.1483.02","url":null,"abstract":"Belogubite, ideally CuZn(SO 4 ) 2 ·10H 2 O, has been found in the supergene zone uncovered by the open pit at the Gayskoe massive sulfide Zn-Cu deposit (Orenburgskaya region, the South Urals, Russia). It is associated with dietrichite and may contain relics of quartz. Belogubite forms aggregates of blue grains up to 1 mm in size. The mineral is transparent with vitreous luster and white streak. Its color varies from pale equant to light blue. Cleavage and parting were not observed. The new mineral is brittle and has Mohsʼ hardness ca . 2½. Its density measured by floatation in bromoform+ethanol is 2.27(2) g/cm –3 , its calculated density is 2.249 g/cm –3 . Belogubite is biaxial (–), α = 1.512(2), β = 1.525(2), γ = 1.531(2); 2 V (meas.) = 70(10)°, 2 V (calc.) = 67.9°. Dispersion is noticeable, r < v . The mineral is nonpleochroic. Chemical composition of the holotype sample is (wt %, electron microprobe data, H 2 O determined by thermogravimetry): MgO 1.12, MnO 0.10, FeO 3.15, CuO 8.98, ZnO 18.02, SO 3 32.49, H 2 O 36.75, total 100.61. Its empirical formula calculated on the basis of 18 O apfu is: (Cu 0.55 Zn0 .45 ) Σ1.00 (Zn 0.64 Fe 0.22 Mg 0.14 Mn 0.01 ) Σ1.01 S 1.99 O 7.98 ·10.02H 2 O. The structure was solved by direct methods and refined on the basis of 1797 independent reflections to R = 0.016. Belogubite is triclinic, P 1 . Unit cell parameters are: a = 6.2548(1), b = 10.6112(2), c = 6.0439(1) A, α = 82.587(1), β = 109.625(1), γ = 104.848(1)°, V = 364.81(1) A 3 , Z = 1. The strongest reflections of the powder XRD pattern are [ d obs , A ( I ) ( hkl )]: 5.73 (35) (100), 5.576 (47) (–110), 4.873 (100) (–111), 3.907 (31) (021), 3.719 (45) (0 –21), 3.229 (27) (111), 2.915 (25) (–221), 2.684 (26) (130). Belogubite is a new, CuZn-ordered member of the chalcanthite group having M 1 cationic site preferentially occupied by Cu whereas M 2 site is dominated by Zn with subordinate substitution of Fe 2+ and Mg. The mineral is named in honor of Elena Vitalievna Belogub (born 1963), major researcher of the Institute of Mineralogy of the Urals Branch of Russian Academy of Sciences, Miass, Chelyabinsk Oblast, Russia, a well-known expert in the mineralogy of volcanic-hosted massive sulfide copper deposits of South Urals.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69567419","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2019-01-01DOI: 10.30695/zrmo/2019.1481.07
V. D.A., Ermolaeva V.N., C. N.V., Jančev S., Vigasina M.F., Plechov P.Y.
{"title":"New data on chemical composition and Raman spectra of epidote-supergroup minerals","authors":"V. D.A., Ermolaeva V.N., C. N.V., Jančev S., Vigasina M.F., Plechov P.Y.","doi":"10.30695/zrmo/2019.1481.07","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1481.07","url":null,"abstract":"","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":"9 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69565691","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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