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Highly siderophile elements in Earth, Mars, the Moon, and asteroids
The highly siderophile elements (HSE: Os, Ir, Ru, Rh, Pt, Pd, Re, Au) are key tracers of
planetary accretion and differentiation processes due to their affinity for metal relative to …
planetary accretion and differentiation processes due to their affinity for metal relative to …
[HTML][HTML] Elemental and isotopic variability in solar system materials by mixing and processing of primordial disk reservoirs
Isotope anomalies among planetary bodies provide key constraints on planetary genetics
and the solar system's dynamical evolution. However, to unlock the full potential of these …
and the solar system's dynamical evolution. However, to unlock the full potential of these …
[HTML][HTML] Precious and structural metals on asteroids
KM Cannon, M Gialich, J Acain - Planetary and Space Science, 2023 - Elsevier
Metals and metallic elements in silicate/oxide form are abundant in asteroid materials and
are often touted as a valuable space resource that can be returned to Earth or used in …
are often touted as a valuable space resource that can be returned to Earth or used in …
Chemical characteristics of iron meteorite parent bodies
CD Hilton, RD Ash, RJ Walker - Geochimica et Cosmochimica Acta, 2022 - Elsevier
The projected relative abundances of the highly siderophile elements (HSE; Re, Os, Ir, Ru,
Pt, and Pd) for bulk parent bodies of 10 magmatic iron meteorite groups/grouplet (IC, IIAB …
Pt, and Pd) for bulk parent bodies of 10 magmatic iron meteorite groups/grouplet (IC, IIAB …
Nucleosynthetic isotope variations of siderophile and chalcophile elements in the Solar System
Numerous investigations have been devoted to understanding how the materials that
contributed to the Solar System formed, were incorporated into the precursor molecular …
contributed to the Solar System formed, were incorporated into the precursor molecular …
Ultra-depleted 2.05 Ga komatiites of Finnish Lapland: Products of grainy late accretion or core-mantle interaction?
Abstract Rhenium-Os, Ptsingle bondOs, Smsingle bondNd, Lusingle bondHf, and Hfsingle
bond W isotope data, together with lithophile trace element and highly siderophile element …
bond W isotope data, together with lithophile trace element and highly siderophile element …
Building Earth with pebbles made of chondritic components
Pebble accretion provides new insights into Earth's building blocks and early protoplanetary
disk conditions. Here, we show that mixtures of chondritic components: metal grains …
disk conditions. Here, we show that mixtures of chondritic components: metal grains …
Early global mantle chemical and isotope heterogeneity revealed by the komatiite-basalt record: The Western Australia connection
Although the heterogeneous nature of the chemical composition of Earth's mantle is now
well established, the origin and longevity of the heterogeneities continue to be debated. In …
well established, the origin and longevity of the heterogeneities continue to be debated. In …
A 187Re-187Os, 87Rb-87Sr, highly siderophile and incompatible trace element study of some carbonaceous, ordinary and enstatite chondrite meteorites
Abstract New 187 Re-187 Os, 87 Rb-87 Sr, triple O-isotope isotope, bulk rock highly
siderophile-(HSE: Os, Ir, Ru, Pt, Pd, Re), major-and trace-element abundance data are …
siderophile-(HSE: Os, Ir, Ru, Pt, Pd, Re), major-and trace-element abundance data are …
The origin of the unique achondrite Northwest Africa 6704: Constraints from petrology, chemistry and Re–Os, O and Ti isotope systematics
Northwest Africa (NWA) 6704 is a unique achondrite characterized by a near-chondritic
major element composition with a remarkably intact igneous texture. To investigate the …
major element composition with a remarkably intact igneous texture. To investigate the …