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Betzite, Na (sub 6) Ca (sub 2) (Al (sub 6) Si (sub 6) O (sub 24) )C (sub l4) , a new cancrinite-group mineral from the Eifel paleovolcanic region, Germany

Nikita V. Chukanov, Natalia V. Zubkova, Olga N. Kazheva, Dmitry A. Varlamov, Igor V. Pekov, Dmitriy I. Belakovskiy, Bernd Ternes, Willi Schueller, Sergey N. Britvin and Dmitry Yu. Pushcharovsky
Betzite, Na (sub 6) Ca (sub 2) (Al (sub 6) Si (sub 6) O (sub 24) )C (sub l4) , a new cancrinite-group mineral from the Eifel paleovolcanic region, Germany
The Canadian Journal of Mineralogy and Petrology (January 2023) 61 (1): 177-188

Abstract

Betzite, ideally Na (sub 6) Ca (sub 2) (Al (sub 6) Si (sub 6) O (sub 24) )C (sub l4) , a new cancrinite-group mineral, was discovered in a metasomatically altered (pyrometamorphosed) calcic xenolith, hosted by alkaline basalt at the Bellerberg paleovolcano in the Eastern Eifel region, Rhineland-Palatinate, Germany. The associated minerals are anorthite, phlogopite, diopside, grossular, fluorite, calcite, a tobermorite-like mineral, and vanadoallanite-(Ce). Betzite occurs as colorless hexagonal prismatic crystals up to 2 mm long and up to 0.5 mm thick. The new mineral is brittle, with a Mohs' hardness of 5-1/2. Distinct cleavage on {1010} and parting on {0001} are observed. The D (sub meas) = 2.38(2) g/cm (super 3) and D (sub calc) = 2.363 g/cm (super 3) . Betzite is optically uniaxial (+) with omega = 1.528(2) and epsilon = 1.545(3). The IR spectrum is given. The chemical composition of betzite is (wt.%; electron microprobe, H (sub 2) O determined by the modified Penfield method): Na (sub 2) O 11.88, K (sub 2) O 4.82, CaO 10.74, MgO 0.21, A (sub l2) O (sub 3) 27.32, Fe (sub 2) O (sub 3) 0.68, SiO (sub 2) 32.84, SO (sub 3) 1.89, Cl 10.48, H (sub 2) O 1.10, -O identical with Cl -2.37, total 99.59. The empirical formula is Na (sub 4.22) K (sub 1.13) Ca (sub 2.11) Mg (sub 0.06) (Si (sub 6.01) Al (sub 5.90) Fe (super 3+) (sub 0.09) O (sub 24) )Cl (sub 3.2 5) (SO (sub 4) )0.2 (sub 6) (H (sub 1.34) O (sub 0.64) ). The crystal structure was determined using single-crystal X-ray diffraction data. It is hexagonal, space group P6 (sub 3) , a = 12.8166(9) Aa, c = 5.3562(3) Aa, V = 761.95(12) Aa (super 3) 3 (at a temperature of 100 K) and Z = 3. Betzite is a dimorph of quadridavyne, with a disordered distribution of extra-framework components occupying channels. The strongest lines of the powder X-ray diffraction pattern [d, Aa (I, %) (hkl)] are: 11.14 (31) (100), 4.833 (93) (101), 3.715 (95) (300), 3.313 (100) (211), 2.787 (37) (400), 2.681 (56) (002, 131), 2.474 (35) (112, 401), 2.146 (24) (330). The mineral is named in honor of the German amateur mineralogist Volker Betz (b. 1947).


EISSN: 2817-1713
Serial Title: The Canadian Journal of Mineralogy and Petrology
Serial Volume: 61
Serial Issue: 1
Title: Betzite, Na (sub 6) Ca (sub 2) (Al (sub 6) Si (sub 6) O (sub 24) )C (sub l4) , a new cancrinite-group mineral from the Eifel paleovolcanic region, Germany
Affiliation: Russian Academy of Sciences, Federal Research Center of Problems of Chemical Physics and Medicinal Chemistry, Moscow, Russian Federation
Pages: 177-188
Published: 202301
Text Language: English
Publisher: Mineralogical Association of Canada, Ottawa, ON, Canada
References: 26
Accession Number: 2023-023791
Categories: Mineralogy of silicatesIgneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 6 tables
N50°00'00" - N50°30'00", E06°19'60" - E07°19'60"
Secondary Affiliation: Moscow State University, RUS, Russian FederationRussian Academy of Sciences, RUS, Russian FederationSaint Petersburg State University, RUS, Russian Federation
Country of Publication: Canada
Secondary Affiliation: GeoRef, Copyright 2023, American Geosciences Institute. Abstract, copyright, Mineralogical Association of Canada. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 2023
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