Jahnsite-(MnMnZn), a new jahnsite-group mineral, and formal approval of the jahnsite group

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F19%3A00111302" target="_blank" >RIV/00216224:14310/19:00111302 - isvavai.cz</a>

Výsledek na webu

<a href="https://pubs.geoscienceworld.org/eurjmin/article-abstract/31/1/167/548185/Jahnsite-MnMnZn-a-new-jahnsite-group-mineral-and?redirectedFrom=fulltext" target="_blank" >https://pubs.geoscienceworld.org/eurjmin/article-abstract/31/1/167/548185/Jahnsite-MnMnZn-a-new-jahnsite-group-mineral-and?redirectedFrom=fulltext</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/ejm/2018/0030-2800" target="_blank" >10.1127/ejm/2018/0030-2800</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Jahnsite-(MnMnZn), a new jahnsite-group mineral, and formal approval of the jahnsite group

Popis výsledku v původním jazyce

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 &lt; 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 &lt; M2 &lt; M1 &lt; 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).

Název v anglickém jazyce

Jahnsite-(MnMnZn), a new jahnsite-group mineral, and formal approval of the jahnsite group

Popis výsledku anglicky

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 &lt; 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 &lt; M2 &lt; M1 &lt; 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).

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

European Journal of Mineralogy

ISSN

0935-1221

e-ISSN

1617-4011

Svazek periodika

31

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

6

Strana od-do

167-172

Kód UT WoS článku

000460524200016

EID výsledku v databázi Scopus

2-s2.0-85062074160