Highly Siderophile Element and 187Os Signatures in Non-cratonic Basalt-hosted Peridotite Xenoliths: Unravelling the Origin and Evolution of the Post-Archean …
The highly siderophile elements (HSE) consist of the Platinum Group Elements (PGE: Ru,
Rh, Pd, Os, Ir, Pt) along with rhenium and gold. These transition elements show relative …
Rh, Pd, Os, Ir, Pt) along with rhenium and gold. These transition elements show relative …
Gold endowment of the metasomatized lithospheric mantle for giant gold deposits: Insights from lamprophyre dykes
The metasomatized sub-continental lithospheric mantle (SCLM) is increasingly proposed to
play a key control in the formation of giant gold (Au) deposits. However, the extent of Au …
play a key control in the formation of giant gold (Au) deposits. However, the extent of Au …
The roles of various types of crustal contamination in the genesis of the **chuan magmatic Ni-Cu-PGE deposit: New mineralogical and CS-Sr-Nd isotope constraints
Addition of crustal sulfur to the **chuan magma or oxidation of the magma associated with
carbonate assimilation has been considered to be the main cause of sulfide saturation in the …
carbonate assimilation has been considered to be the main cause of sulfide saturation in the …
Se–Te fractionation by sulfide–silicate melt partitioning: implications for the composition of mantle-derived magmas and their melting residues
JM Brenan - Earth and Planetary Science Letters, 2015 - Elsevier
Abstract Partitioning of Se and Te has been measured between coexisting sulfide liquid,
monosulfide solid solution (MSS) and silicate melt at 0.9–1.5 GPa, 1200–1300° C, fO 2 …
monosulfide solid solution (MSS) and silicate melt at 0.9–1.5 GPa, 1200–1300° C, fO 2 …
Sedimentary response to the paleogeographic and tectonic evolution of the southern North China Craton during the late Paleozoic and Mesozoic
With the aim of constraining the influence of the surrounding plates on the Late Paleozoic–
Mesozoic paleogeographic and tectonic evolution of the southern North China Craton …
Mesozoic paleogeographic and tectonic evolution of the southern North China Craton …
[HTML][HTML] Formation of the youngest Ni-Cu sulfide-mineralized intrusion in the Chinese Eastern Tianshan: Constraints from geochronology, PGE geochemistry and Hf …
H Tian, S Xue, H Sun, X Wang, L Wang, X Wang… - Ore Geology …, 2024 - Elsevier
The timing of magmatic sulfide mineralization in orogenic belts is critical for Ni-Cu mineral
exploration. In the Chinese Eastern Tianshan, the Ni-Cu sulfide mineralization is presumed …
exploration. In the Chinese Eastern Tianshan, the Ni-Cu sulfide mineralization is presumed …
Dating mantle peridotites using Re-Os isotopes: The complex message from whole rocks, base metal sulfides, and platinum group minerals
Abstract The Re-Os isotopic system is largely considered the geochronometer of choice to
date partial melting of terrestrial peridotites and in constraining the evolution of Earth's …
date partial melting of terrestrial peridotites and in constraining the evolution of Earth's …
The role of Te, As, Bi, Sn and Sb during the formation of platinum-group-element reef deposits: Examples from the Bushveld and Stillwater Complexes
The distribution of platinum-group element (PGE) and Te, As, Bi, Sb and Sn (TABS) in whole-
rock samples, and in disseminated base metal sulfides (BMS) pentlandite, pyrrhotite and …
rock samples, and in disseminated base metal sulfides (BMS) pentlandite, pyrrhotite and …
Copper isotope fractionation during partial melting and melt percolation in the upper mantle: Evidence from massif peridotites in Ivrea-Verbano Zone, Italian Alps
To investigate the behavior of Cu isotopes during partial melting and melt percolation in the
mantle, we have analyzed Cu isotopic compositions of a suite of well-characterized …
mantle, we have analyzed Cu isotopic compositions of a suite of well-characterized …
Significance of the whole rock Re–Os ages in cryptically and modally metasomatised cratonic peridotites: Constraints from HSE–Se–Te systematics
Abstract The Re–Os isotopic system is the geochronometer of choice to constrain the timing
of lithospheric mantle root formation and reconstruct the evolution of Earth's dynamics from …
of lithospheric mantle root formation and reconstruct the evolution of Earth's dynamics from …