• journal_title：American Mineralogist
• Contributor：José González Del Tánago ; Ángel La Iglesia ; Jordi Rius ; Soledad Fernández Santín
• Publisher：Mineralogical Society of America
• Date：2003-
• Format：text/html
• Language：en
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：88
• issue：11-12
• firstpage：1703
• section：Articles

Calderonite, ideally Pb₂Fe³⁺(VO₄)₂(OH), a new member of the brackebuschite group, has been found in the upper oxidation zone of two Pb-Zn hydrothermal deposits located at Santa Marta and Azuaga, Badajoz province, Spain. Brackebuschite and calderonite probably form a complete solid solution, locally with important substitution of Cu and Zn for Fe and Mn. The monoclinic cell parameters derived from powder X-ray diffraction (XRD) data are: a = 7.647(5) Å, b = 6.094(1) Å, c = 8.900(2) Å, β = 112.0(2)° and V = 384.5(4) ų, and the six strongest lines, d-spacing (Å),(I),(hkl), are: 4.893(4)(011), 4.166(3)(002), 3.242(10) (2̅11), 3.058(3)(020), 2.980(5) (1̅03) and 2.746(5)(003). Electron microprobe analyses (EMPA) show a certain degree of compositional variation not only between the Santa Marta and Azuaga samples but also among grains from the same locality. A representative formula of Santa Marta calderonite, determined from EMPA, based on 9 O atoms: is (Pb_1.950Ca_0.004Ba_0.015)_1.969(Fe³⁺_0.892Cu_0.059Zn_0.008Al_0.015)_0.974 (V_1.847As_0.008Si_0.039P_0.057)_1.951O_7.507(OH)_1.493. Fe³⁺ is principally substituted by Cu²⁺, and V⁵⁺ by Si⁴⁺. ρ_c = 6.05 g/cm³. The thermogravimetric analysis yields a weight loss of 1.91%, which corresponds to the 1.493 H needed to maintain the charge balance. Differential thermal analysis shows endothermic effects at 279 and 663 °C due to dehydroxylation.

A single-crystal XRD refinement was carried out on a selected crystal with cationic content determined by EMPA and starting atomic positions from brackebuschite. Final R-value of 5.81% based on 952 reflections with I > 2σ_I, assuming P2₁/m symmetry, the cell dimensions are a = 7.649 Å, b = 6.101 Å, c = 8.904 Å, β = 112.23°.

Calderonite is red orange to red brown, semitransparent to translucent with vitreous luster and red streak and powder. The fracture is splintery. Optically, it is biaxial positive, with a 2V_X = 86° and strong dispersion. In plane-polarized light, it is strongly pleochroic (X = light greenish brown, Y = brown, Z = reddish brown).