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Murashkoite, FeP, a new terrestrial phosphide from pyrometamorphic rocks of the Hatrurim Formation, South Levant.

Authors :
Britvin, Sergey N.
Vapnik, Yevgeny
Polekhovsky, Yury S.
Krivovichev, Sergey V.
Krzhizhanovskaya, Maria G.
Gorelova, Liudmila A.
Vereshchagin, Oleg S.
Shilovskikh, Vladimir V.
Zaitsev, Anatoly N.
Source :
Mineralogy & Petrology; Apr2019, Vol. 113 Issue 2, p237-248, 12p
Publication Year :
2019

Abstract

Murashkoite, FeP, is a new mineral found in pyrometamorphic rocks of the Hatrurim Formation, South Levant. It is a typical accessory phase in the marbles and paralavas in the southern Negev Desert, Israel and on the Transjordan Plateau, Jordan. Murashkoite occurs as grains and aggregates up to 2 mm closely associated with barringerite, (Fe,Ni)<subscript>2</subscript>P, and zuktamrurite, FeP<subscript>2</subscript>. The rock-forming minerals include pyroxenes of the diopside-hedenbergite series, anorthite with subordinate gehlenite, tridymite, cristobalite, pyrrhotite, fluorapatite, chromite, magnetite, hematite, merrillite and late hydrothermal carbonates, silicates and sulfates. Macroscopically, murashkoite is yellowish-grey in colour and has a metallic lustre. In reflected light, the mineral is white with a beige tint and it is non-pleochroic. The anisotropy is distinct, from yellow-grey to greyish-blue. Selected reflectance values [R<subscript>max</subscript>-R<subscript>min</subscript>, % (λ, nm)] are: 42.7-40.8 (400), 42.0-40.6 (500), 44.5-43.4 (600), 48.0-47.7 (700). It is brittle. VHN<subscript>20</subscript> = 468 kg mm<superscript>−2</superscript>. The holotype material has the chemical composition (electron microprobe): Fe 63.82; Ni 0.88; P 35.56; total 100.26 wt.%. The empirical formula calculated on the basis of 2 apfu is (Fe<subscript>0.99</subscript>Ni<subscript>0.01</subscript>)<subscript>1.00</subscript>P<subscript>1.00</subscript> corresponding to FeP. Murashkoite is orthorhombic, space group Pnma, unit cell parameters refined from the single-crystal data are: a 5.099(2), b 3.251(2), c 5.695(2) Å, V 94.41(8) Å<superscript>3</superscript>, Z = 4, D<subscript>x</subscript> = 6.108(5) g cm<superscript>−3</superscript>. The crystal structure was solved and refined to R<subscript>1</subscript> = 0.0305 on the basis of 131 unique reflections with I > 2σ(I). The strongest lines of the powder X-ray diffraction pattern [(d, Å) (I, %) (hkl)]: 2.831(75)(002,011); 2.548(22)(200); 2.477(46)(102,111); 1.975(47)(112); 1.895(100)(202,211); 1.779(19)(103); 1.632(45)(013,301,020). The mineral is named in honour of Dr. Mikhail Nikolaevich Murashko (born 1952), for his contributions to the mineralogy of the Hatrurim Formation. Murashkoite is a natural counterpart of synthetic FeP, the compound widely used in heterogeneous catalysis and electrocatalysis. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
09300708
Volume :
113
Issue :
2
Database :
Complementary Index
Journal :
Mineralogy & Petrology
Publication Type :
Academic Journal
Accession number :
135395071
Full Text :
https://doi.org/10.1007/s00710-018-0647-y