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31.
Murzin V. V. Badanina I. Yu. Malitch K. N. Ignatiev A. V. Velivetskaya T. A. 《Doklady Earth Sciences》2019,488(1):1097-1099
Doklady Earth Sciences - This study presents the first data set of sulfur isotope compositions of primary Ru–Os sulfides, represented by laurite (RuS2) – erlichmanite (OsS2) series,... 相似文献
32.
The composition and isotopic-geochemical peculiarities of zircons from the ore-bearing ultramafic-mafic intrusions of western Taimyr that are promising for finding Pt-Cu-Ni mineralization were characterized for the first time. The similar U-Pb age of zircons from the Binyuda and Dyumaltei intrusions (248.3 ± 13 and 244.4 ± 2.4 Ma, respectively) indicates that the intrusions were formed almost synchronously with tholeiitic basalts of the Siberian Platform. The age and Nd-Sr data of intrusions of western Taimyr are distinct from those of economic ore-bearing intrusions of the Noril’sk province characterized by long-term magmatic evolution of the rocks and different material sources. 相似文献
33.
Summary ?We report, for the first time, the occurrence of five palladium-rich, one palladium bearing and two gold-silver minerals
from podiform chromitites in the Eastern Alps. Minerals identified include braggite, keithconnite, stibiopalladinite, potarite,
mertieite II, Pd-bearing Pt-Fe alloy, native gold and Ag-Au alloy. They occur in heavy mineral concentrates produced from
two massive podiform chromitite samples (unaltered and highly altered) of the Kraubath ultramafic massif, Styria, Austria.
Distribution patterns of platinum-group elements (PGE) in these chromitites show considerable differences in the behaviour
of the less refractory PGE (PPGE-group: Rh, Pt, Pd) compared to the refractory PGE (IPGE-group: Os, Ir, Ru). PPGE are more
enriched in chromitite showing pronounced alteration features. The unaltered chromitite displays a negatively sloped chondrite-normalised
PGE pattern similar to typical ophiolitic-podiform chromitite.
Except for the Pd- and Au-Ag minerals that are generally rare in ophiolites, about 20 other platinum-group minerals (PGM)
have been discovered. They include PGE-sulphides (laurite, erlichmanite, kashinite, bowieite, cuproiridsite, cuprorhodsite,
unnamed Ir-rich variety of ferrorhodsite, unnamed Ni-Fe-Cu-Rh- and Ni-Fe-Cu-Ir-Rh monosulphides), PGE alloys (Pt-Fe, Ir-Os,
Os-Ir and Ru-Os-Ir), PGE-sulpharsenides (irarsite, hollingworthite, platarsite, ruarsite and a number of intermediate species),
sperrylite and a Ru-rich oxide (?). Three PGM assemblages have been recognised and attributed to different processes ranging
from magmatic to hydrothermal and weathering-related.
Pd-rich minerals are characteristic of both chromitite types, although their chemistry and relative proportions vary considerably.
Keithconnite, braggite and Pd-bearing ferroan platinum, together with a number of PGE-sulphides (mainly laurite-erlichmanite)
and alloys, are typical only of the unaltered podiform chromitite (assemblage I). Euhedral mono- and polyphase PGM grains
in the submicron to 100 μm range show features of primary magmatic assemblages. The diversity of PGM in these assemblages
is unusual for ophiolitic environments. In assemblage II, laurite-erlichmanite is intergrown with and overgrown by PGE-sulpharsenides;
other minerals of assemblage I are missing. Potarite, stibiopalladinite, mertieite II, native gold and Ag-Au alloys, as well
as PGE-sulpharsenides, sperrylite and base metal arsenides and sulphides are characteristic for the highly altered chromitite
(assemblage III). They occur either interstitial to chromite in association with metamorphic silicates, in chromite rims or
along cracks, and are thus interpreted as having formed by remobilization of PGE by hydrothermal processes during polyphase
regional metamorphism.
Received August 3, 2000;/revised version accepted December 28, 2000 相似文献