Isomorphism in vanadinite. 1. Chemical variation and solid solutions
- 作者: Karpov A.O.1,2, Agakhanov A.A.2, Pekov I.V.1
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隶属关系:
- Moscow State University
- Fersman Mineralogical Museum RAS
- 期: 卷 CLIII, 编号 5 (2024)
- 页面: 127-155
- 栏目: МИНЕРАЛОГИЧЕСКАЯ КРИСТАЛЛОГРАФИЯ
- URL: https://journals.rcsi.science/0869-6055/article/view/281296
- DOI: https://doi.org/10.31857/S0869605524050079
- EDN: https://elibrary.ru/PCEAZO
- ID: 281296
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The chemical composition of hundred vanadinite specimens from 17 occurrences worldwide was studied by electron microprobe and the new and literature data on its chemical composition were summarized. Vanadinite is a supergene mineral: no reliable data indicating that vanadinite may be hypogene have been found, although its analogue is synthesized in a wide temperature range: from 25 to 1000 °C. The overwhelming majority of vanadinite specimens have a composition close to the ideal formula, Pb5(VO4)3Cl. Phosphorus and/or arsenic-rich vanadinite (> 0.5 apfu P and/or As) is rare, as well as a Cr-bearing variety of this mineral. According to the data available today, isomorphism between V, As and P in natural vanadinite–pyromorphite–mimetite system is incomplete unlike synthetic system Pb5(T5+O4)3Cl (T = V, P, As) in which full miscibility occurs, even at low temperatures. For the vanadinite–mimetite series, the compositional range from V3.00As0.00 to As2.15V0.85 has been recorded while the vanadinite–pyromorphite series is so far represented almost only by the vanadinite part: from V3.00P0.00 to P1.50V1.50. Two new finds of the so-called endlichite (an intermediate member of the vanadinite–mimetite series with a V: As ratio of ~1:1, data on which were previously based only on wet chemical analyses published in 1885) were made. The calcium content in all vanadinite samples studied in this work does not exceed 0.2 apfu, and the contents of other elements with atomic numbers >8, excepting Pb, Ca, V, P, As and Cl, are below their detection limits by electron microprobe.
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作者简介
A. Karpov
Moscow State University; Fersman Mineralogical Museum RAS
编辑信件的主要联系方式.
Email: karpovao@my.msu.ru
Faculty of Geology, Moscow State University
俄罗斯联邦, Moscow; MoscowA. Agakhanov
Fersman Mineralogical Museum RAS
Email: karpovao@my.msu.ru
俄罗斯联邦, Moscow
I. Pekov
Moscow State University
Email: karpovao@my.msu.ru
Faculty of Geology
俄罗斯联邦, Moscow参考
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