Add to ORKGWe investigated Re-Os for whole rocks, sulfide, and metal from ordinary chondrites. Reproducible analyses for Re/Os in chondrites are obtained. Data on St. Séverin (LL6) show a large range in ^(187)Re/^(188)OS (0.31-0.78) and in ^(187)OS/^(188)OS (0.119-0.157)
Rhenium (Re) is one of the least abundant elements in Earth, averaging 0.28 ppb in the primitive man...
This study aims to better characterize highly siderophile element (HSE; Re, Os, Ir, Ru, Pt and Pd) a...
To evaluate the homogeneity of geological reference material BIR-1a (basalt; United States Geologica...
We have investigated the Re-Os system for samples of whole rock, metal, and sulfide from ordinary ch...
Abstract—The Re-Os isotopic systematics of calcium–aluminium-rich inclusions (CAIs) in chondrites we...
In the past two decades, the 187Re-187Os system, as other common radiogenic isotope systems, has bee...
The Re-Os system for samples of FeNi, sulphide, and phosphide from iron meteorites was investigated....
International audienceNew 187Re-187Os, 87Rb-87Sr, triple O-isotope isotope, bulk rock highly siderop...
We investigated Re-Os for whole rocks, sulfide, and metal from ordinary chondrites. Reproducible ana...
The St-Robert H5 chondrite yields a mineral/whole-rock Pb-Pb age of 4565 +/- 23 Ma (2-sigma) compara...
The 187Re-187Os isotopic systematics of many bulk chondrites plot well beyond analytical uncertainti...
A new development on the measurement of the Os isotopic composition by mass spectrometry using negat...
Although Earth's continental crust is thought to derive from melting of the Earth's mantle, how the ...
Coupled 187Os/188Os compositions and highly-siderophile-element (HSE: Os, Ir, Ru, Pt, Pd, and Re) ab...
This study uses Re-Os isotopes from sulfide minerals (molybdenite, pyrite, chalcopyrite, bornite, sp...
Rhenium (Re) is one of the least abundant elements in Earth, averaging 0.28 ppb in the primitive man...
This study aims to better characterize highly siderophile element (HSE; Re, Os, Ir, Ru, Pt and Pd) a...
To evaluate the homogeneity of geological reference material BIR-1a (basalt; United States Geologica...
We have investigated the Re-Os system for samples of whole rock, metal, and sulfide from ordinary ch...
Abstract—The Re-Os isotopic systematics of calcium–aluminium-rich inclusions (CAIs) in chondrites we...
In the past two decades, the 187Re-187Os system, as other common radiogenic isotope systems, has bee...
The Re-Os system for samples of FeNi, sulphide, and phosphide from iron meteorites was investigated....
International audienceNew 187Re-187Os, 87Rb-87Sr, triple O-isotope isotope, bulk rock highly siderop...
We investigated Re-Os for whole rocks, sulfide, and metal from ordinary chondrites. Reproducible ana...
The St-Robert H5 chondrite yields a mineral/whole-rock Pb-Pb age of 4565 +/- 23 Ma (2-sigma) compara...
The 187Re-187Os isotopic systematics of many bulk chondrites plot well beyond analytical uncertainti...
A new development on the measurement of the Os isotopic composition by mass spectrometry using negat...
Although Earth's continental crust is thought to derive from melting of the Earth's mantle, how the ...
Coupled 187Os/188Os compositions and highly-siderophile-element (HSE: Os, Ir, Ru, Pt, Pd, and Re) ab...
This study uses Re-Os isotopes from sulfide minerals (molybdenite, pyrite, chalcopyrite, bornite, sp...
Rhenium (Re) is one of the least abundant elements in Earth, averaging 0.28 ppb in the primitive man...
This study aims to better characterize highly siderophile element (HSE; Re, Os, Ir, Ru, Pt and Pd) a...
To evaluate the homogeneity of geological reference material BIR-1a (basalt; United States Geologica...