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

Result code in 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>

Result on the web

<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>

Result language

angličtina

Original language name

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

Original language description

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).

Czech name

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Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10504 - Mineralogy

Project

—

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2019

Confidentiality

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

Name of the periodical

European Journal of Mineralogy

ISSN

0935-1221

e-ISSN

1617-4011

Volume of the periodical

31

Issue of the periodical within the volume

1

Country of publishing house

DE - GERMANY

Number of pages

6

Pages from-to

167-172

UT code for WoS article

000460524200016

EID of the result in the Scopus database

2-s2.0-85062074160