The isotope geochemistry of zinc and copper

F Moynier, D Vance, T Fujii… - Reviews in Mineralogy …, 2017 - pubs.geoscienceworld.org
Copper, a native metal found in ores, is the principal metal in bronze and brass. It is a
reddish metal with a density of 8920 kg m− 3. All of copper's compounds tend to be brightly …

Mass fractionation laws, mass-independent effects, and isotopic anomalies

N Dauphas, EA Schauble - Annual Review of Earth and …, 2016 - annualreviews.org
Isotopic variations usually follow mass-dependent fractionation, meaning that the relative
variations in isotopic ratios scale with the difference in mass of the isotopes involved (eg …

[图书][B] Stable isotope geochemistry

J Hoefs, J Hoefs - 2009 - Springer
The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

Principles of stable isotope geochemistry

Z Sharp - 2017 - digitalrepository.unm.edu
Abstract Principles of Stable Isotope Geochemistry is written as a textbook to accompany a
one semester course in Stable Isotope Geochemistry. There are 13 chapters, each dealing …

Oxygen isotopic evidence for vigorous mixing during the Moon-forming giant impact

ED Young, IE Kohl, PH Warren, DC Rubie… - Science, 2016 - science.org
Earth and the Moon are shown here to have indistinguishable oxygen isotope ratios, with a
difference in Δ′ 17O of− 1±5 parts per million (2 standard error). On the basis of these data …

[HTML][HTML] Water in the Moon's interior: Truth and consequences

EH Hauri, AE Saal, MJ Rutherford… - Earth and Planetary …, 2015 - Elsevier
Geochemical data for H 2 O and other volatiles, as well as major and trace elements, are
reported for 377 samples of lunar volcanic glass from three chemical groups (A15 green …

[HTML][HTML] Rubidium isotopic composition of the Earth, meteorites, and the Moon: Evidence for the origin of volatile loss during planetary accretion

EA Pringle, F Moynier - Earth and Planetary Science Letters, 2017 - Elsevier
Understanding the origin of volatile element variations in the inner Solar System has long
been a goal of cosmochemistry, but many early studies searching for the fingerprint of …

Oxygen isotope identity of the Earth and Moon with implications for the formation of the Moon and source of volatiles

M Fischer, STM Peters, D Herwartz, P Hartogh… - Proceedings of the …, 2024 - pnas.org
The Moon formed 4.5 Ga ago through a collision between proto-Earth and a planetesimal
known as Theia. The compositional similarity of Earth and Moon puts tight limits on the …

Melting and mixing states of the Earth's mantle after the Moon-forming impact

M Nakajima, DJ Stevenson - Earth and Planetary Science Letters, 2015 - Elsevier
Abstract The Earth's Moon is thought to have formed by an impact between the Earth and an
impactor around 4.5 billion years ago. This impact could have been so energetic that it could …

Copper isotope evidence for large-scale sulphide fractionation during Earth's differentiation

PS Savage, F Moynier, H Chen… - Geochemical …, 2015 - research-repository.st-andrews.ac …
The differentiation of Earth into a metallic core and silicate mantle left its signature on the
chemical and isotopic composition of the bulk silicate Earth (BSE). This is seen in the …