Crystal-chemical relations and classification problems in tourmalines belonging to the oxy-schorl-oxy-dravite-bosiite-povondraite series

被引:15
作者
Bosi, Ferdinando [1 ]
Camara, Fernando [2 ,3 ]
Ciriotti, Marco E. [4 ]
Halenius, Ulf [5 ]
Reznitskii, Leonid [6 ]
Stagno, Vincenzo [1 ]
机构
[1] Sapienza Univ Roma, Dipartimento Sci Terra, Piazzale Aldo Moro 5, I-00185 Rome, Italy
[2] Univ Torino, Dipartimento Sci Terra, Via Tommaso Valperga Caluso 35, I-10125 Turin, Italy
[3] CrisDi, Interdept Ctr Res & Dev Crystallog, Via Pietro Giuria 5, I-10125 Turin, Italy
[4] Assoc Micromineral Italiana, Via San Pietro 55, I-10073 Turin, Italy
[5] Swedish Museum Nat Hist, Dept Geosci, Box 50007, S-10405 Stockholm, Sweden
[6] Russian Acad Sci, Siberian Branch, Inst Earths Crust, Lermontova Str 128, Irkutsk, Russia
关键词
tourmaline; crystal-structure refinement; electron microprobe; optical absorption spectroscopy; synchrotron Mssbauer source spectroscopy; nomenclature; DARASUN GOLD DEPOSIT; CHROMIUM-DRAVITE; RICH TOURMALINE; VALLETTA MINE; MAIRA VALLEY; FERRIC-IRON; MAS NMR; CHEMISTRY; BEARING; SREF;
D O I
10.1127/ejm/2017/0029-2616
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Two oxy-tourmalines showing intermediate compositions between the oxy-schorl and oxy-dravite series (sample from Sludyanka crystalline complex, Baikal, Russia) and the oxy-dravite and bosiite series (sample from the Valletta mine, Piedmont, Italy) were structurally and chemically characterized by single-crystal X-ray diffraction, electron microprobe analysis, optical absorption and Synchrotron Mossbauer source spectroscopy. A comparative analysis of the results, along with data from literature on additional samples corresponding to the species oxy-schorl, oxy-dravite, bosiite and povondraite, show that the main structural variations within the Fe-bearing, Na-dominant oxy-tourmalines are related to variations in the content of Fe, which is incorporated into the structure via substitution mechanisms that involves Al. The results also show the occurrence of a complete substitution series from oxy-schorl via oxy-dravite and bosiite to povondraite, but no (or a limited) direct substitution series between oxy-schorl and bosiite (or povondraite). The substitution of Al by larger cations causes changes in < Y-O > and < Z-O > distances as well as in the unit-cell parameters. The effect of < Y-O > on the a-parameter is evident in the oxy-schorl-oxy-dravite series, but it is of marginal significance in the oxy-dravitebosiite- povondraite series. On the other hand, a good correlation exists between < Z-O > and the a-parameter only in the oxy-dravitebosiite- povondraite series. The c-parameter is strongly correlated with < Z-O > along the entire substitution series. Classification problems related to the naming of Fe-bearing, Na-dominant oxy-tourmalines are discussed. Application of the nomenclature rules in force resulted in ambiguous naming of the studied samples. This makes, for example, direct comparisons of physical and chemical properties of tourmalines originating from different deposits difficult.
引用
收藏
页码:445 / 455
页数:11
相关论文
共 63 条
[1]   Oxy-schorl, Na(Fe22+Al)Al6Si6O18(BO3)3(OH)3O, a new mineral from Zlata Idka, Slovak Republic and Pribyslavice, Czech Republic [J].
Bacik, Peter ;
Cempirek, Jan ;
Uher, Pavel ;
Novak, Milan ;
Ozdin, Daniel ;
Filip, Jan ;
Skoda, Radek ;
Breiter, Karel ;
Klementova, Mariana ;
Duda, Rudolf ;
Groat, Lee A. .
AMERICAN MINERALOGIST, 2013, 98 (2-3) :485-492
[2]   FERRIC-IRON-RICH TOURMALINE FROM THE DARASUN GOLD DEPOSIT, TRANSBAIKALIA, RUSSIA [J].
Baksheev, Ivan A. ;
Prokof'ev, Vsevolod Yu. ;
Yapaskurt, Vasily O. ;
Vigasina, Marina F. ;
Zorina, Lidiya D. ;
Solov'ev, Victor N. .
CANADIAN MINERALOGIST, 2011, 49 (01) :263-276
[3]   Linking structure and chemistry in the Schorl-Dravite series [J].
Bloodaxe, ES ;
Hughes, JM ;
Dyar, MD ;
Grew, ES ;
Guidotti, CV .
AMERICAN MINERALOGIST, 1999, 84 (5-6) :922-928
[4]   Crystal chemistry of the elbaite-schorl series [J].
Bosi, F ;
Andreozzi, GB ;
Federico, M ;
Graziani, G ;
Lucchesi, S .
AMERICAN MINERALOGIST, 2005, 90 (11-12) :1784-1792
[5]   Crystal chemistry of the dravite-chromdravite series [J].
Bosi, F ;
Lucchesi, S ;
Reznitskii, L .
EUROPEAN JOURNAL OF MINERALOGY, 2004, 16 (02) :345-352
[6]   Crystal chemistry of the schorl-dravite series [J].
Bosi, F ;
Lucchesi, S .
EUROPEAN JOURNAL OF MINERALOGY, 2004, 16 (02) :335-344
[7]   Bond-valence constraints around the O1 site of tourmaline [J].
Bosi, F. .
MINERALOGICAL MAGAZINE, 2013, 77 (03) :343-351
[8]   Octahedrally coordinated vacancies in tourmaline: a theoretical approach [J].
Bosi, F. .
MINERALOGICAL MAGAZINE, 2010, 74 (06) :1037-1044
[9]   Crystal chemical relationships in the tourmaline group: Structural constraints on chemical variability [J].
Bosi, Ferdinando ;
Lucchesi, Sergio .
AMERICAN MINERALOGIST, 2007, 92 (07) :1054-1063
[10]   Thermal stability of extended clusters in dravite: a combined EMP, SREF and FTIR study [J].
Bosi, Ferdinando ;
Skogby, Henrik ;
Balic-Zunic, Tonci .
PHYSICS AND CHEMISTRY OF MINERALS, 2016, 43 (06) :395-407