KAMPF, Anthony R., Pedro ALVES, Anatoly KASATKIN a Radek ŠKODA. Jahnsite-(MnMnZn), a new jahnsite-group mineral, and formal approval of the jahnsite group. European Journal of Mineralogy. Stuttgart: E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG, 2019, roč. 31, č. 1, s. 167-172. ISSN 0935-1221. Dostupné z: https://dx.doi.org/10.1127/ejm/2018/0030-2800.
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Základní údaje
Originální název Jahnsite-(MnMnZn), a new jahnsite-group mineral, and formal approval of the jahnsite group
Autoři KAMPF, Anthony R., Pedro ALVES, Anatoly KASATKIN a Radek ŠKODA (203 Česká republika, garant, domácí).
Vydání European Journal of Mineralogy, Stuttgart, E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG, 2019, 0935-1221.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10504 Mineralogy
Stát vydavatele Německo
Utajení není předmětem státního či obchodního tajemství
WWW URL
Impakt faktor Impact factor: 1.665
Kód RIV RIV/00216224:14310/19:00111302
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1127/ejm/2018/0030-2800
UT WoS 000460524200016
Klíčová slova anglicky Jahnsite-(MnMnZn); new mineral; jahnsite-group; crystal structure; Raman spectroscopy; Herdade dos Pendoes mine; Portugal
Štítky rivok
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: Mgr. Marie Šípková, DiS., učo 437722. Změněno: 26. 3. 2020 13:47.
Anotace
Jahnsite-(MnNInZn) (IMA2017-113), Mn(2)(2+)Zn2Fe(3)(2+)(PO4)(4)(OH)(2) center dot 8H(2)O, is a new member of the jahnsite group from the Herdade dos Pendries mine, Beja district, southwest Portugal. It formed in a highly altered gossan in association with Zn-bearing libethenite, quartz, rhodochrosite and santabarbaraite. It occurs in sub-parallel bundles of light golden brown prisms up to 0.3 mm long. Crystals are transparent with vitreous to silky lustre and white streak. The mineral is brittle with irregular, splintery fracture, good cleavage parallel to {001} and Mohs' hardness of about 4. The measured density is 2.89(2) g cm(-3). Optically, it is biaxial (+), with alpha = 1.655(2), beta = 1.662(2), gamma = 1.673(2) (white light); 2V = 78(1)degrees; pleochroism: X nearly colourless, Y and Z beige; X < Y approximate to Z. Electron microprobe analyses gave the empirical formula (Mn0.712+Na0.15Ca0.10)Sigma(0.96) (Mn-1.00(2+)) (Zn1.00Mn0.662+Fe0.212+Mg0.10Fe0.033+)(Sigma 2.00)(Fe1.993+Al0.01)(Sigma 2.00)(P1.01O4)(4)(OH)(2) center dot 8H(2)O. Jahnsite-(MnMnZn) is monoclinic, P2/a, a = 15.222(6), b = 7.187(6), c = 10.028(5) angstrom, beta = 111.746(16)degrees, V = 1019.0(11) angstrom(3) and Z = 2. The eight strongest lines in the X-ray powder diffraction pattern are [d(obs)/angstrom (I) (hkl)]: 9.25 (63) (001), 5.00 (40) (210,21 (1) over bar ,111), 4.648 (33) (002), 3.509 (41) (40 (2) over bar), 2.842 (100) (022), 1.9984 (37) (422,42 (4) over bar), 1.9506 (30) (024) and 1.5853 (33) (820,82 (4) over bar). The jahnsite group has now been officially established by the Commission on New Minerals, Nomenclature and Classification. The general formula for jahnsite-group minerals is XM1M2(2)M3(2)(H2O)(8)(OH)(2)(PO4)(4); the ionic radii for the cation sites generally increase as follows: M3 < M2 < M1 < X, and the M3 site determines whether the species belongs to the jahnsite subgroup (M3 = Fe3+) or the whiteite subgroup (M3 = Al). The subgroup name is generally used as the species root name to be followed by a suffix of the form-(XM1M2). Using this as a guide for the jahnsite described herein results in the following site assignments: X = Mn, M1 = Mn, M2 = Zn, and M3 = Fe; and the name jahnsite-(MnMnZn).
VytisknoutZobrazeno: 29. 7. 2024 08:03