Magnesium isotope geochemistry
FZ Teng - Reviews in Mineralogy and Geochemistry, 2017 - pubs.geoscienceworld.org
Magnesium (Mg) has an atomic number of 12 and belongs to the alkaline earth element
(Group II) of the Periodic Table. The pure Mg is a silvery white metal and has a melting point …
(Group II) of the Periodic Table. The pure Mg is a silvery white metal and has a melting point …
Garnet: A rock-forming mineral petrochronometer
EF Baxter, MJ Caddick… - Reviews in Mineralogy …, 2017 - pubs.geoscienceworld.org
Garnet could be the ultimate petrochronometer. Not only can you date it directly (with an
accuracy and precision that may surprise some), but it is also a common rock-forming and …
accuracy and precision that may surprise some), but it is also a common rock-forming and …
Assessment of international reference materials for isotope-ratio analysis (IUPAC Technical Report)
Since the early 1950s, the number of international measurement standards for anchoring
stable isotope delta scales has mushroomed from 3 to more than 30, expanding to more …
stable isotope delta scales has mushroomed from 3 to more than 30, expanding to more …
Iron isotopic compositions of geological reference materials and chondrites
PR Craddock, N Dauphas - Geostandards and Geoanalytical …, 2011 - Wiley Online Library
High‐precision iron isotopic compositions for Fe‐bearing geological reference materials and
chondrites with a wide range of matrices (eg, silicates, oxides, organic‐bearing materials) …
chondrites with a wide range of matrices (eg, silicates, oxides, organic‐bearing materials) …
Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present
High-precision Fe isotopic data for 104 samples, including modern and ancient (≥ 3.7 Ga)
subduction-related magmas and mantle peridotites, are presented. These data demonstrate …
subduction-related magmas and mantle peridotites, are presented. These data demonstrate …
Iron, zinc, magnesium and uranium isotopic fractionation during continental crust differentiation: The tale from migmatites, granitoids, and pegmatites
The causes of some stable isotopic variations in felsic rocks are not well understood. In
particular, the origin of the heavy Fe isotopic compositions (ie, high δ56Fe values, deviation …
particular, the origin of the heavy Fe isotopic compositions (ie, high δ56Fe values, deviation …
Iron isotopic systematics of oceanic basalts
The iron isotopic compositions of 93 well-characterized basalts from geochemically and
geologically diverse mid-ocean ridge segments, oceanic islands and back arc basins were …
geologically diverse mid-ocean ridge segments, oceanic islands and back arc basins were …
High-temperature equilibrium isotope fractionation of non-traditional stable isotopes: Experiments, theory, and applications
High-temperature partitioning of the stable isotopes of rock-forming elements like Mg, Si, Fe,
Ni and others are useful new tools in geochemistry and cosmochemistry. Understanding the …
Ni and others are useful new tools in geochemistry and cosmochemistry. Understanding the …
Secular mantle oxidation across the Archean-Proterozoic boundary: Evidence from V partitioning in komatiites and picrites
The oxygen fugacities of nine mantle-derived komatiitic and picritic systems ranging in age
from 3.55 Ga to modern day were determined using the redox-sensitive partitioning of V …
from 3.55 Ga to modern day were determined using the redox-sensitive partitioning of V …
The effect of bonding environment on iron isotope fractionation between minerals at high temperature
PA Sossi, HSC O'Neill - Geochimica et Cosmochimica Acta, 2017 - Elsevier
Central to understanding the processes that drive stable isotope fractionation in nature is
their quantification under controlled experimental conditions. The polyvalent element iron …
their quantification under controlled experimental conditions. The polyvalent element iron …