2021
DOI: 10.3749/canmin.2100002
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Palladothallite, Pd3Tl, a new mineral from the Monchetundra layered intrusion, Kola Peninsula, Russia

Abstract: Palladothallite, Pd3Tl, is a new mineral discovered in the Monchetundra layered intrusion, Kola Peninsula, Russia. Palladothallite occurs in orthopyroxenite with disseminated Ni-Cu-Fe sulfides and in near-surface oxidized ore of an orthopyroxenite unit. In the holotype specimen, the new mineral forms anhedral grains about 1 to 20 μm in size intergrown with bortnikovite (Pt4Cu3Zn). Palladothallite and bortnikovite form a rim around tulameenite (Pt2FeCu), Pt-Pd-Fe-Cu alloys, and Pt-Pd-Fe-Cu “oxides” in a goethit… Show more

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Cited by 3 publications
(2 citation statements)
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“…The transferability of these bonding schemes among the structures hints that analogous pictures can be drawn for other group 10 metalbased compounds. We are looking forward to seeing how similar bonding configurations may be used to unify the broader structural chemistry [13][14][15][16][17] of this family of intermetallic phases.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The transferability of these bonding schemes among the structures hints that analogous pictures can be drawn for other group 10 metalbased compounds. We are looking forward to seeing how similar bonding configurations may be used to unify the broader structural chemistry [13][14][15][16][17] of this family of intermetallic phases.…”
Section: Discussionmentioning
confidence: 99%
“…In this Article, we will consider the structure of Pd 5 InAs as an instance of such a situation, in which a preferred stacking arrangement reveals key bonding features. This compound represents a broader family of group 10 element-rich intermetallics incorporating AuCu 3 -type units [13][14][15][16][17] and has previously been explored for its potential to host hydrogen. [18] It adopts the Pd 5 TlAs structure type (Figure 1), [19][20][21] in which 1-unit-cell thick slabs of the AuCu 3 type and layers of edge-sharing filled square prisms derived from the PtHg 2 type [22] (or its stacking variant, the fluorite type) [23] alternate along the c direction.…”
Section: Introductionmentioning
confidence: 99%