PAŠAVAITE, Pd3Pb2Te2, a new platinum-group mineral species from Noril`sk-Talnakh Ni-Cu camp, Russia

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F09%3A00000022" target="_blank" >RIV/00025798:_____/09:00000022 - isvavai.cz</a>

Alternative codes found

RIV/00023272:_____/09:#0000990 RIV/00216208:11310/09:00014524

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

PAŠAVAITE, Pd3Pb2Te2, a new platinum-group mineral species from Noril`sk-Talnakh Ni-Cu camp, Russia

Original language description

Pašavaite, Pd3Pb2Te2, is a new palladium mineral species discovered at the Talnakh deposit, Noril`sk-Talnakh Ni-Cu camp, Taimyr Autonomous District, Russia. It was observed in two polished sections, where it occurs as subhedral grains not exceeding 20 ?min diameter embedded in polarite, and randomly accompanied by unknown Pd-Pb-Bi-Te phases and sperylite or intergrown with Au-Ag phases. In plane-polarized light, pašavaite is pale pink with brownish tinge, has strong bireflectance, pleochroic from brownish to light pink, distinctly to strongly anisotropic, and exhibits no internal reflections. The mineral is orthorhombic, space group Pmmn, with a 8.599(1), b 5.9381(6), c 6.3173(8) A, V 322.6(1) A3 and Z = 2. The crystal structure was solved and refinedfrom the powder X-ray diffraction data of syntetic Pd3Pb2Te2.

Czech name

Pašavait, Pd3Pb2Te2, nový minerál ze skupiny minerálů Pt-kovů z ložiska Norilsk - Talnach, Rusko

Czech description

Pašavaite, Pd3Pb2Te2, is a new palladium mineral species discovered at the Talnakh deposit, Noril`sk-Talnakh Ni-Cu camp, Taimyr Autonomous District, Russia. It was observed in two polished sections, where it occurs as subhedral grains not exceeding 20 ?min diameter embedded in polarite, and randomly accompanied by unknown Pd-Pb-Bi-Te phases and sperylite or intergrown with Au-Ag phases. In plane-polarized light, pašavaite is pale pink with brownish tinge, has strong bireflectance, pleochroic from brownish to light pink, distinctly to strongly anisotropic, and exhibits no internal reflections. The mineral is orthorhombic, space group Pmmn, with a 8.599(1), b 5.9381(6), c 6.3173(8) A, V 322.6(1) A3 and Z = 2. The crystal structure was solved and refinedfrom the powder X-ray diffraction data of syntetic Pd3Pb2Te2.

Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

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Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year

2009

Confidentiality

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

Name of the periodical

Canadian Mineralogist

ISSN

0008-4476

e-ISSN

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Volume of the periodical

47

Issue of the periodical within the volume

1

Country of publishing house

CA - CANADA

Number of pages

10

Pages from-to

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UT code for WoS article

265004800005

EID of the result in the Scopus database

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