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Evidence of fluid-induced myrmekite formation after alkali-feldspar megacryst: example from a metaporphyritic granitoid in Makrohar, Madhya Pradesh, India 碱性长石巨晶后流体诱发麦饭石形成的证据:印度中央邦马克罗哈尔的元斑状花岗岩实例
IF 2.7 3区 地球科学 Q2 MINERALOGY Pub Date : 2023-11-30 DOI: 10.1180/mgm.2023.90
Arimita Chakrabarty, Shreya Karmakar, U. Dutta, Sanjoy Sanyal, P. Sengupta
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引用次数: 0
Characterization, axial anisotropy and formation conditions of celestine from the Jabal Eghei (Nuqay) late Neogene – Pleistocene volcanic province, southern Libya: Constraints on the mineralogical geothermometer 利比亚南部 Jabal Eghei(Nuqay)新近纪-更新世晚期火山省的天青石的特征、轴向各向异性和形成条件:矿物学地温计的制约因素
IF 2.7 3区 地球科学 Q2 MINERALOGY Pub Date : 2023-11-28 DOI: 10.1180/mgm.2023.88
P. Tančić, Maja Milošević, D. Spahić, Bojan Kostić, Aleksandar Kremenović, Maja Poznanović-Spahić, Jovan Kovačević
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引用次数: 0
A new mineral cuprodobrovolskyite Na4Cu(SO4)3 from the Tolbachik volcano (Kamchatka, Russia) and the relations in the family of natural anhydrous Na-Cu sulfates 俄罗斯托尔巴切克火山新矿物Na4Cu(SO4)3及其在天然无水钠铜硫酸盐家族中的关系
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-11-13 DOI: 10.1180/mgm.2023.85
Nadezhda V. Shchipalkina, Igor V. Pekov, Natalia N. Koshlyakova, Dmitry I. Belakovskiy, Natalia V. Zubkova, Atali A. Agakhanov, Sergey N. Britvin, Maria A. Nazarova
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引用次数: 1
Bimbowrieite, NaMgFe3+5(PO4)4(OH)6⋅2H2O, a new dufrénite-group mineral from the White Rock No.2 quarry, South Australia, Australia. Bimbowrieite, NaMgFe3+5(PO4)4(OH)6⋅2H2O,是一种来自澳大利亚南澳大利亚White Rock 2号采石场的新dufrsamuite族矿物。
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-11-13 DOI: 10.1180/mgm.2023.86
Peter Elliott, Anthony R. Kampf
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引用次数: 0
Celebrating the International Year of Mineralogy Progress and Landmark Discoveries of the Last Decades Editors: Luca Bindi, Giuseppe Cruciani 庆祝国际矿物学进步年和过去几十年的里程碑式发现编辑:Luca Bindi, Giuseppe crucani
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-23 DOI: 10.1180/mgm.2023.79
Gurmeet Kaur
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引用次数: 0
2023 list of referees for Mineralogical Magazine 《矿物学杂志》2023年评审人名单
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-16 DOI: 10.1180/mgm.2023.81
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引用次数: 0
Tellurium-rich stibiogoldfieldite and Se-bearing dantopaite from Goldfield, Nevada, U.S.A.: new crystal chemical data 美国内华达州金矿区富碲辉生金矿石和含硒辉生金矿石:新的晶体化学数据
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-16 DOI: 10.1180/mgm.2023.77
Silvia MUSETTI, Jiří SEJKORA, Cristian BIAGIONI, Zdeněk DOLNÍČEK
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引用次数: 0
The oxidation state and distribution of Fe in pumpellyite from the Northern Chichibu Belt in the Hijikawa district, western Shikoku, Japan 日本四国西部Hijikawa地区北秩父带中铁的氧化态和分布
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-16 DOI: 10.1180/mgm.2023.80
Masahide Akasaka, Yumi Goishi (Imaizumi), Masayuki Sakakibara, Yoshihiro Nakamuta
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{"title":"The oxidation state and distribution of Fe in pumpellyite from the Northern Chichibu Belt in the Hijikawa district, western Shikoku, Japan","authors":"Masahide Akasaka, Yumi Goishi (Imaizumi), Masayuki Sakakibara, Yoshihiro Nakamuta","doi":"10.1180/mgm.2023.80","DOIUrl":"https://doi.org/10.1180/mgm.2023.80","url":null,"abstract":"An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.","PeriodicalId":18618,"journal":{"name":"Mineralogical Magazine","volume":"11 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-10-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136113196","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Okruginite, Cu2SnSe3, a new mineral from the Ozernovskoe deposit, Kamchatka peninsula, Russia 俄罗斯堪察加半岛Ozernovskoe矿床新矿物Cu2SnSe3 - Okruginite
3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-16 DOI: 10.1180/mgm.2023.78
Anna Vymazalová, Vladimir V. Kozlov, František Laufek, Chris J. Stanley, Ilya A. Shkilev, Sharapat Kudaeva, Filip Košek
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{"title":"Okruginite, Cu<sub>2</sub>SnSe<sub>3</sub>, a new mineral from the Ozernovskoe deposit, Kamchatka peninsula, Russia","authors":"Anna Vymazalová, Vladimir V. Kozlov, František Laufek, Chris J. Stanley, Ilya A. Shkilev, Sharapat Kudaeva, Filip Košek","doi":"10.1180/mgm.2023.78","DOIUrl":"https://doi.org/10.1180/mgm.2023.78","url":null,"abstract":"An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.","PeriodicalId":18618,"journal":{"name":"Mineralogical Magazine","volume":"74 3 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-10-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136113523","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Kalyuzhnyite-(Ce), NaKCaSrCeTi(Si8O21)OF(H2O)3, a new mineral from the Darai-Pioz alkaline massif, Tien-Shan mountains, Tajikistan: mineral description, crystal structure and a new double (Si8O21) sheet 塔吉克斯坦天山Darai-Pioz碱性丘陵的新矿物Kalyuzhnyite-(Ce),NaKCaSrCeTi(Si8O21)OF(H2O)3:矿物描述、晶体结构和新的双(Si8O21)薄片
IF 2.7 3区 地球科学 Q2 MINERALOGY Pub Date : 2023-10-13 DOI: 10.1180/mgm.2023.74
Atali A. Agakhanov, Elena Sokolova, Vladimir Yu. Karpenko, Frank C. Hawthorne, Leonid A. Pautov, Anatoly V. Kasatkin, Igor V. Pekov, Vitaliya A. Agakhanova
<p>Kalyuzhnyite-(Ce), ideally NaKCaSrCeTi(Si<span>8</span>O<span>21</span>)OF(H<span>2</span>O)<span>3</span>, is a new mineral from the Darai-Pioz alkaline massif, Tien-Shan mountains, Tajikistan. It occurs as equant grains up to 0.05 × 0.07 mm in a quartz–pectolite aggregate in a silexite-like peralkaline pegmatite. Associated minerals are quartz, fluorite, pectolite, baratovite, aegirine, leucosphenite, neptunite, reedmergnerite, orlovite, sokolovaite, mendeleevite-(Ce), odigitriaite, pekovite, zeravshanite, kirchhoffite and garmite. The mineral is colourless with a vitreous lustre and a white streak, and <span>D</span><span>calc.</span> is 3.120 g/cm<span>3</span>. Kalyuzhnyite-(Ce) is monoclinic, <span>P</span>2/<span>c</span>, <span>a</span> = 18.647(4), <span>b</span> = 11.214(2), <span>c</span> = 14.642(3) Å, β = 129.55(3)° and <span>V</span> = 2360.9(11) Å<span>3</span>. The chemical composition of kalyuzhnyite-(Ce) is Nb<span>2</span>O<span>5</span> 0.53, TiO<span>2</span> 0.16, SiO<span>2</span> 43.85, Er<span>2</span>O<span>3</span> 0.13, Ho<span>2</span>O<span>3</span> 0.10, Gd<span>2</span>O<span>3</span> 0.09, Sm<span>2</span>O<span>3</span> 0.47, Nd<span>2</span>O<span>3</span> 6.22, Pr<span>2</span>O<span>3</span> 1.21, Ce<span>2</span>O<span>3</span> 6.34, La<span>2</span>O<span>3</span> 0.82, PbO 4.90, BaO 0.85, SrO 11.39, CaO 1.86, Cs<span>2</span>O 3.80, K<span>2</span>O 1.59, Na<span>2</span>O 2.99, H<span>2</span>O 5.24, F 1.55, O = F –0.65, total 100.31 wt.%. The empirical formula calculated on 26.11 (O + F) apfu is Na<span>1.07</span>K<span>0.37</span>Cs<span>0.30</span>Sr<span>1.21</span>Ca<span>0.37</span>Pb<span>0.24</span>Ba<span>0.06</span>(Ce<span>0.43</span>Nd<span>0.41</span>Pr<span>0.08</span>La<span>0.06</span>Sm<span>0.03</span>Gd<span>0.01</span>Er<span>0.01</span>Ho<span>0.01</span>)<span>Σ1.04</span>(Ti<span>0.97</span>Nb<span>0.04</span>)<span>Σ1.01</span>Si<span>8.06</span>O<span>25.21</span>F<span>0.90</span>H<span>6.42</span>, <span>Z</span> = 4. The simplified formula is (Na,□)(K,Сs)(Ca,Pb,Sr,Na)Sr<span>Ln</span><span>3+</span>Ti(Si<span>8</span>O<span>21</span>)OF(H<span>2</span>O)<span>3</span>, where Ce is the dominant lanthanoid. The crystal structure was solved by direct methods and refined to an <span>R</span><span>1</span> index of 2.74%. In kalyuzhnyite-(Ce), the main structural units are a heteropolyhedral Na–Sr–Ce–Ti sheet, ideally [NaSrCeTiOF]<span>7+</span>, and a double (Si<span>8</span>O<span>21</span>)<span>10–</span> sheet parallel to (010). In the Si–O sheet, the Si tetrahedra form ten-membered rings. This is the first occurrence of such a double Si–O sheet in a mineral. The two sheets connect via common vertices of Na-, Sr-, Ce- and Ti-polyhedra and SiO<span>4</span> tetrahedra to form a framework. The interstitial cations and H<span>2</span>O groups, ideally [(CaK)(H<span>2</span>O)<span>3</span>]<span>3+</span><span>,</span> occur within the Si–O sheet. The mineral is named in honour
Kalyuzhnyite-(Ce),理想状态为 NaKCaSrCeTi(Si8O21)OF(H2O)3,是一种产自塔吉克斯坦天山Darai-Pioz碱性地块的新矿物。它以最大 0.05 × 0.07 毫米的等粒形式出现在石英-埃洛石集合体中,位于一个类似围岩的伟晶岩中。伴生矿物有石英、萤石、pectolite、baratovite、aegirine、leucosphenite、neptunite、reedmergnerite、orlovite、sokolovaite、mendeleevite-(Ce)、odigitriaite、pekovite、zeravshanite、kirchhoffite 和 garmite。该矿物无色,具有玻璃光泽和白色条纹,密度为 3.120 克/立方厘米。Kalyuzhnyite-(Ce)呈单斜,P2/c,a = 18.647(4),b = 11.214(2),c = 14.642(3)埃,β = 129.55(3)°,V = 2360.9(11)埃3。kalyuzhnyite-(Ce)的化学成分为 Nb2O5 0.53、TiO2 0.16、SiO2 43.85、Er2O3 0.13、Ho2O3 0.10、Gd2O3 0.09、Sm2O3 0.47、Nd2O3 6.22、Pr2O3 1.21, Ce2O3 6.34, La2O3 0.82, PbO 4.90, BaO 0.85, SrO 11.39, CaO 1.86, Cs2O 3.80, K2O 1.59, Na2O 2.99, H2O 5.24, F 1.55, O = F -0.65, 总计 100.31 wt.%。根据 26.11 (O + F) apfu 计算得出的经验公式为 Na1.07K0.37Cs0.30Sr1.21Ca0.37Pb0.24Ba0.06(Ce0.43Nd0.41Pr0.08La0.06Sm0.03Gd0.01Er0.01Ho0.01)Σ1.04(Ti0.97Nb0.04)Σ1.01Si8.06O25.21F0.90H6.42, Z = 4.简化公式为 (Na,□)(K,Сs)(Ca,Pb,Sr,Na)SrLn3+Ti(Si8O21)OF(H2O)3,其中 Ce 是主要的镧系元素。该晶体结构是通过直接方法求解的,其 R1 指数为 2.74%。在 kalyuzhnyite-(Ce)中,主要的结构单元是异多面体 Na-Sr-Ce-Ti 片(理想状态为 [NaSrCeTiOF]7+)和平行于 (010) 的双 (Si8O21)10- 片。在 Si-O 片层中,Si 四面体形成十元环。这是矿物中首次出现这种双 Si-O 片层。两个薄片通过 Na-、Sr-、Ce- 和 Ti- 多面体以及 SiO4 四面体的共同顶点连接起来,形成一个框架。间隙阳离子和 H2O 基团(理想情况下为[(CaK)(H2O)3]3+)出现在 Si-O 片层中。该矿物以 Vasily Avksentievich Kalyuzhny(1899-1993 年)命名,以表彰他对苏联科米共和国矿床地质学和塔吉克斯坦花岗伟晶岩矿物学的贡献。
{"title":"Kalyuzhnyite-(Ce), NaKCaSrCeTi(Si8O21)OF(H2O)3, a new mineral from the Darai-Pioz alkaline massif, Tien-Shan mountains, Tajikistan: mineral description, crystal structure and a new double (Si8O21) sheet","authors":"Atali A. Agakhanov, Elena Sokolova, Vladimir Yu. Karpenko, Frank C. Hawthorne, Leonid A. Pautov, Anatoly V. Kasatkin, Igor V. Pekov, Vitaliya A. Agakhanova","doi":"10.1180/mgm.2023.74","DOIUrl":"https://doi.org/10.1180/mgm.2023.74","url":null,"abstract":"&lt;p&gt;Kalyuzhnyite-(Ce), ideally NaKCaSrCeTi(Si&lt;span&gt;8&lt;/span&gt;O&lt;span&gt;21&lt;/span&gt;)OF(H&lt;span&gt;2&lt;/span&gt;O)&lt;span&gt;3&lt;/span&gt;, is a new mineral from the Darai-Pioz alkaline massif, Tien-Shan mountains, Tajikistan. It occurs as equant grains up to 0.05 × 0.07 mm in a quartz–pectolite aggregate in a silexite-like peralkaline pegmatite. Associated minerals are quartz, fluorite, pectolite, baratovite, aegirine, leucosphenite, neptunite, reedmergnerite, orlovite, sokolovaite, mendeleevite-(Ce), odigitriaite, pekovite, zeravshanite, kirchhoffite and garmite. The mineral is colourless with a vitreous lustre and a white streak, and &lt;span&gt;D&lt;/span&gt;&lt;span&gt;calc.&lt;/span&gt; is 3.120 g/cm&lt;span&gt;3&lt;/span&gt;. Kalyuzhnyite-(Ce) is monoclinic, &lt;span&gt;P&lt;/span&gt;2/&lt;span&gt;c&lt;/span&gt;, &lt;span&gt;a&lt;/span&gt; = 18.647(4), &lt;span&gt;b&lt;/span&gt; = 11.214(2), &lt;span&gt;c&lt;/span&gt; = 14.642(3) Å, β = 129.55(3)° and &lt;span&gt;V&lt;/span&gt; = 2360.9(11) Å&lt;span&gt;3&lt;/span&gt;. The chemical composition of kalyuzhnyite-(Ce) is Nb&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;5&lt;/span&gt; 0.53, TiO&lt;span&gt;2&lt;/span&gt; 0.16, SiO&lt;span&gt;2&lt;/span&gt; 43.85, Er&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 0.13, Ho&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 0.10, Gd&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 0.09, Sm&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 0.47, Nd&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 6.22, Pr&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 1.21, Ce&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 6.34, La&lt;span&gt;2&lt;/span&gt;O&lt;span&gt;3&lt;/span&gt; 0.82, PbO 4.90, BaO 0.85, SrO 11.39, CaO 1.86, Cs&lt;span&gt;2&lt;/span&gt;O 3.80, K&lt;span&gt;2&lt;/span&gt;O 1.59, Na&lt;span&gt;2&lt;/span&gt;O 2.99, H&lt;span&gt;2&lt;/span&gt;O 5.24, F 1.55, O = F –0.65, total 100.31 wt.%. The empirical formula calculated on 26.11 (O + F) apfu is Na&lt;span&gt;1.07&lt;/span&gt;K&lt;span&gt;0.37&lt;/span&gt;Cs&lt;span&gt;0.30&lt;/span&gt;Sr&lt;span&gt;1.21&lt;/span&gt;Ca&lt;span&gt;0.37&lt;/span&gt;Pb&lt;span&gt;0.24&lt;/span&gt;Ba&lt;span&gt;0.06&lt;/span&gt;(Ce&lt;span&gt;0.43&lt;/span&gt;Nd&lt;span&gt;0.41&lt;/span&gt;Pr&lt;span&gt;0.08&lt;/span&gt;La&lt;span&gt;0.06&lt;/span&gt;Sm&lt;span&gt;0.03&lt;/span&gt;Gd&lt;span&gt;0.01&lt;/span&gt;Er&lt;span&gt;0.01&lt;/span&gt;Ho&lt;span&gt;0.01&lt;/span&gt;)&lt;span&gt;Σ1.04&lt;/span&gt;(Ti&lt;span&gt;0.97&lt;/span&gt;Nb&lt;span&gt;0.04&lt;/span&gt;)&lt;span&gt;Σ1.01&lt;/span&gt;Si&lt;span&gt;8.06&lt;/span&gt;O&lt;span&gt;25.21&lt;/span&gt;F&lt;span&gt;0.90&lt;/span&gt;H&lt;span&gt;6.42&lt;/span&gt;, &lt;span&gt;Z&lt;/span&gt; = 4. The simplified formula is (Na,□)(K,Сs)(Ca,Pb,Sr,Na)Sr&lt;span&gt;Ln&lt;/span&gt;&lt;span&gt;3+&lt;/span&gt;Ti(Si&lt;span&gt;8&lt;/span&gt;O&lt;span&gt;21&lt;/span&gt;)OF(H&lt;span&gt;2&lt;/span&gt;O)&lt;span&gt;3&lt;/span&gt;, where Ce is the dominant lanthanoid. The crystal structure was solved by direct methods and refined to an &lt;span&gt;R&lt;/span&gt;&lt;span&gt;1&lt;/span&gt; index of 2.74%. In kalyuzhnyite-(Ce), the main structural units are a heteropolyhedral Na–Sr–Ce–Ti sheet, ideally [NaSrCeTiOF]&lt;span&gt;7+&lt;/span&gt;, and a double (Si&lt;span&gt;8&lt;/span&gt;O&lt;span&gt;21&lt;/span&gt;)&lt;span&gt;10–&lt;/span&gt; sheet parallel to (010). In the Si–O sheet, the Si tetrahedra form ten-membered rings. This is the first occurrence of such a double Si–O sheet in a mineral. The two sheets connect via common vertices of Na-, Sr-, Ce- and Ti-polyhedra and SiO&lt;span&gt;4&lt;/span&gt; tetrahedra to form a framework. The interstitial cations and H&lt;span&gt;2&lt;/span&gt;O groups, ideally [(CaK)(H&lt;span&gt;2&lt;/span&gt;O)&lt;span&gt;3&lt;/span&gt;]&lt;span&gt;3+&lt;/span&gt;&lt;span&gt;,&lt;/span&gt; occur within the Si–O sheet. The mineral is named in honour","PeriodicalId":18618,"journal":{"name":"Mineralogical Magazine","volume":"48 5 1","pages":""},"PeriodicalIF":2.7,"publicationDate":"2023-10-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139771716","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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Mineralogical Magazine
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