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@article{fe4a36c49779449499055ac05f6ba49e,
title = "Ekplexite (Nb, Mo)S-2 center dot(Mg1-xAlx)(OH)(2+x), kaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) and manganokaskasite (Mo, Nb)S-2 center dot(Mn1-xAlx)(OH)(2+x), three new valleriite-group mineral species from the Khibiny alkaline complex, Kola peninsula, Russia",
abstract = "Three new valleriite-group minerals, ekplexite (Nb, Mo)S-2 center dot(Mg1-xAlx)(OH)(2+x), kaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) and manganokaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) are found at Mt Kaskasnyunchorr, Khibiny alkaline complex, Kola Peninsula, Russia. They occur in fenite consisting of orthoclase-anorthoclase and nepheline with fluorophlogopite, corundum, pyrrhotite, pyrite, rutile, monazite-(Ce), graphite, edgarite, molybdenite, tungstenite, alabandite, etc. Ekplexite forms lenticular nests up to 0.2 mm x 1 mm x 1 mm consisting of near-parallel, radiating or chaotic aggregates of flakes. Kaskasite and manganokaskasite mainly occur as flakes and their near-parallel 'stacks' (kaskasite: up to 0.03 mm x 1 mm x 1.5 mm; manganokaskasite: up to 0.02 mm x 0.5 mm x 1 mm) epitaxially overgrow Ti-bearing pyrrhotite partially replaced by Ti-bearing pyrite. All three new minerals are opaque, iron-black, with metallic lustre. Cleavage is {001} perfect and mica-like. Flakes are very sof",
author = "Pekov, {I. V.} and Yapaskurt, {V. O.} and Polekhovsky, {Y. S.} and Vigasina, {M. F.} and Siidra, {O. I.}",
year = "2014",
doi = "10.1180/minmag.2014.078.3.14",
language = "English",
volume = "78",
pages = "663--679",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "3",

}

RIS

TY - JOUR

T1 - Ekplexite (Nb, Mo)S-2 center dot(Mg1-xAlx)(OH)(2+x), kaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) and manganokaskasite (Mo, Nb)S-2 center dot(Mn1-xAlx)(OH)(2+x), three new valleriite-group mineral species from the Khibiny alkaline complex, Kola peninsula, Russia

AU - Pekov, I. V.

AU - Yapaskurt, V. O.

AU - Polekhovsky, Y. S.

AU - Vigasina, M. F.

AU - Siidra, O. I.

PY - 2014

Y1 - 2014

N2 - Three new valleriite-group minerals, ekplexite (Nb, Mo)S-2 center dot(Mg1-xAlx)(OH)(2+x), kaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) and manganokaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) are found at Mt Kaskasnyunchorr, Khibiny alkaline complex, Kola Peninsula, Russia. They occur in fenite consisting of orthoclase-anorthoclase and nepheline with fluorophlogopite, corundum, pyrrhotite, pyrite, rutile, monazite-(Ce), graphite, edgarite, molybdenite, tungstenite, alabandite, etc. Ekplexite forms lenticular nests up to 0.2 mm x 1 mm x 1 mm consisting of near-parallel, radiating or chaotic aggregates of flakes. Kaskasite and manganokaskasite mainly occur as flakes and their near-parallel 'stacks' (kaskasite: up to 0.03 mm x 1 mm x 1.5 mm; manganokaskasite: up to 0.02 mm x 0.5 mm x 1 mm) epitaxially overgrow Ti-bearing pyrrhotite partially replaced by Ti-bearing pyrite. All three new minerals are opaque, iron-black, with metallic lustre. Cleavage is {001} perfect and mica-like. Flakes are very sof

AB - Three new valleriite-group minerals, ekplexite (Nb, Mo)S-2 center dot(Mg1-xAlx)(OH)(2+x), kaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) and manganokaskasite (Mo, Nb)S-2 center dot(Mg1-xAlx)(OH)(2+x) are found at Mt Kaskasnyunchorr, Khibiny alkaline complex, Kola Peninsula, Russia. They occur in fenite consisting of orthoclase-anorthoclase and nepheline with fluorophlogopite, corundum, pyrrhotite, pyrite, rutile, monazite-(Ce), graphite, edgarite, molybdenite, tungstenite, alabandite, etc. Ekplexite forms lenticular nests up to 0.2 mm x 1 mm x 1 mm consisting of near-parallel, radiating or chaotic aggregates of flakes. Kaskasite and manganokaskasite mainly occur as flakes and their near-parallel 'stacks' (kaskasite: up to 0.03 mm x 1 mm x 1.5 mm; manganokaskasite: up to 0.02 mm x 0.5 mm x 1 mm) epitaxially overgrow Ti-bearing pyrrhotite partially replaced by Ti-bearing pyrite. All three new minerals are opaque, iron-black, with metallic lustre. Cleavage is {001} perfect and mica-like. Flakes are very sof

U2 - 10.1180/minmag.2014.078.3.14

DO - 10.1180/minmag.2014.078.3.14

M3 - Article

VL - 78

SP - 663

EP - 679

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 3

ER -

ID: 7031819