• journal_title：Mineralogical Magazine
• Contributor：E. Sokolova ; Y. Abdu ; F. C. Hawthorne ; A. V. Stepanov ; G. K. Bekenova ; P. E. Kotel'nikov
• Publisher：Mineralogical Society of Great Britain and Ireland
• Date：2009-
• Format：text/html
• Language：en
• Identifier：10.1180/minmag.2009.073.5.847
• journal_abbrev：Mineralogical Magazine
• issn：0026-461X
• volume：73
• issue：5
• firstpage：847
• section：Articles

Cámaraite, ideally Ba₃NaTi₄(Fe²⁺,Mn)₈(Si₂O₇)₄O₄(OH,F)₇, is a new mineral from the Verkhnee Espe deposit, Akjailyautas Mountains, Kazakhstan. It occurs as intergrowths with bafertisite and jinshajiangite in separate platy crystals up to 8 mm × 15 mm × 2 mm in size, or as star-shaped aggregates of crystals with different orientations. Individual crystals are orange-red to brownish-red, and are platy on {001}. Cámaraite is translucent and has a pale-yellow streak, a vitreous lustre, and does not fluoresce under cathode or ultraviolet light. Cleavage is {001} perfect, no parting was observed, and Mohs hardness is <5; the mineral is brittle. The calculated density is 4.018 g cm^-3. In transmitted light, cámaraite is strongly pleochroic, X = light brown, Y = reddish-brown, Z = yellow-brown, with Z < X < Y. Cámaraite is biaxial +ve and 2V_meas. = 93(1)°. All refractive indices are greater than 1.80. Cámaraite is triclinic, space group Class="inline-formula" id="inline-formula-1">lass="math tex" alt="Formula" src="847/embed/tex-math-1.gif" />, a = 10.678(4) Å, b = 13.744(8) Å, c = 21.40(2) Å, α = 99.28(8)°, β = 92.38(5)°, γ = 90.00(6)°, V = 3096(3) ų, Z = 4, a:b:c = 0.7761:1:1.5565. The seven strongest lines in the X-ray powder-diffraction pattern are as follows: [d (Å), (I), (hkl)]: 2.63, (100), (401); 2.79, (90), (lass="inline-formula" id="inline-formula-2">lass="math tex" alt="Formula" src="847/embed/tex-math-2.gif" />lass="inline-formula" id="inline-formula-3">lass="math tex" alt="Formula" src="847/embed/tex-math-3.gif" />3, lass="inline-formula" id="inline-formula-4">lass="math tex" alt="Formula" src="847/embed/tex-math-4.gif" />41, 2lass="inline-formula" id="inline-formula-5">lass="math tex" alt="Formula" src="847/embed/tex-math-5.gif" />6, 225); 1.721, (70), (lass="inline-formula" id="inline-formula-6">lass="math tex" alt="Formula" src="847/embed/tex-math-6.gif" />lass="inline-formula" id="inline-formula-7">lass="math tex" alt="Formula" src="847/embed/tex-math-7.gif" />11, lass="inline-formula" id="inline-formula-8">lass="math tex" alt="Formula" src="847/embed/tex-math-8.gif" />49, 0lass="inline-formula" id="inline-formula-9">lass="math tex" alt="Formula" src="847/embed/tex-math-9.gif" />2); 3.39, (50), (2lass="inline-formula" id="inline-formula-10">lass="math tex" alt="Formula" src="847/embed/tex-math-10.gif" />4, 223); 3.18, (50), (lass="inline-formula" id="inline-formula-11">lass="math tex" alt="Formula" src="847/embed/tex-math-11.gif" />lass="inline-formula" id="inline-formula-12">lass="math tex" alt="Formula" src="847/embed/tex-math-12.gif" />5, lass="inline-formula" id="inline-formula-13">lass="math tex" alt="Formula" src="847/embed/tex-math-13.gif" />24); 2.101, (50), (lass="inline-formula" id="inline-formula-14">lass="math tex" alt="Formula" src="847/embed/tex-math-14.gif" />lass="inline-formula" id="inline-formula-15">lass="math tex" alt="Formula" src="847/embed/tex-math-15.gif" />2, lass="inline-formula" id="inline-formula-16">lass="math tex" alt="Formula" src="847/embed/tex-math-16.gif" />40); 1.578, (50), (lass="inline-formula" id="inline-formula-17">lass="math tex" alt="Formula" src="847/embed/tex-math-17.gif" />lass="inline-formula" id="inline-formula-18">lass="math tex" alt="Formula" src="847/embed/tex-math-18.gif" />1, lass="inline-formula" id="inline-formula-19">lass="math tex" alt="Formula" src="847/embed/tex-math-19.gif" />lass="inline-formula" id="inline-formula-20">lass="math tex" alt="Formula" src="847/embed/tex-math-20.gif" />2, 6lass="inline-formula" id="inline-formula-21">lass="math tex" alt="Formula" src="847/embed/tex-math-21.gif" />1, lass="inline-formula" id="inline-formula-22">lass="math tex" alt="Formula" src="847/embed/tex-math-22.gif" />40). Chemical analysis by electron microprobe gave: Nb₂O₅ 1.57, SiO₂ 25.25, TiO₂ 15.69, ZrO₂ 0.33, Al₂O₃ 0.13, Fe₂O₃ 2.77, FeO 16.54, MnO 9.46, ZnO 0.12, MgO 0.21, CaO 0.56, BaO 21.11, Na₂O 1.41, K₂O 0.84, H₂O 1.84, F 3.11, less O ≡ F 1.31, total 99.63 wt.%, where the valence state of Fe was determined by Mössbauer spectroscopy [Fe³⁺/(Fe²⁺ + Fe³⁺) = 0.13(8)] and the H₂O content was derived by crystal-structure determination. The resulting empirical formula on the basis of 39 anions is (Ba_2.61K_0.34)_Σ2.95(Na_0.86Ca_0.14)_Σ1(Ti_3.72Nb_0.22Al_0.05)_Σ3.99(lass="inline-formula" id="inline-formula-23">lass="math tex" alt="Formula" src="847/embed/tex-math-23.gif" />lass="inline-formula" id="inline-formula-24">lass="math tex" alt="Formula" src="847/embed/tex-math-24.gif" />Mn_2.53Mg_0.10Zr_0.05Zn_0.03Ca_0.05)_Σ7.78Si_7.97O_35.89H_3.88F_3.11. Cámaraite is a Group-II TS-block mineral in the structure hierarchy of Sokolova (lass="xref-bibr">2006). The mineral is named cámaraite after Fernando Cámara (born 1967) of Melilla, Spain, in recognition of his contribution to the fields of mineralogy and crystallography. The new mineral and mineral name have been approved by the Commission on New Minerals, Nomenclature and Classification, International Mineralogical Association (IMA 2009-11).