Heidi E. Höfer
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View article: Mélange Signatures and Low Oxygen Fugacity in Eclogite Xenoliths From the Crust‐Mantle Transition Below a Mesoproterozoic Collision Belt
Mélange Signatures and Low Oxygen Fugacity in Eclogite Xenoliths From the Crust‐Mantle Transition Below a Mesoproterozoic Collision Belt Open
Mass transfer across the crust‐mantle boundary is a fundamental process governing planetary differentiation, the evolution of geochemical reservoirs and ore formation, controlled by physicochemical conditions at the crust‐mantle interface.…
View article: A fast open data reduction workflow for the electron microprobe flank method to determine Fe3+/ΣFe contents in minerals
A fast open data reduction workflow for the electron microprobe flank method to determine Fe3+/ΣFe contents in minerals Open
Knowing the Fe 3+ /SFe ratio in minerals is important to understand the formation and evolution of minerals and their host rocks.Variable Fe 3+ /SFe in e.g., garnet is accompanied by a change of their characteristic FeLa and FeLb X-ray emi…
View article: A new web-based and open data reduction application to determine Fe2+/Fe3+ ratios using the electron microprobe flank method.
A new web-based and open data reduction application to determine Fe2+/Fe3+ ratios using the electron microprobe flank method. Open
The electron microprobe (EPMA) flank method can be used to determine in-situ the Fe2+/Fe3+ ratios in garnet [1], and potentially also in other minerals. It is a tool to reveal the redox history of rocks, especially when the garnet grain si…
View article: A web-based, open tool for the preparation and data reduction of electron microprobe measurements.
A web-based, open tool for the preparation and data reduction of electron microprobe measurements. Open
View article: Behaviour of S and Fe during multi-stage metasomatism of oceanic crust as revealed by eclogite xenoliths from the Colorado Plateau
Behaviour of S and Fe during multi-stage metasomatism of oceanic crust as revealed by eclogite xenoliths from the Colorado Plateau Open
View article: Accessories in Kaiserstuhl carbonatites and related rocks as accurate and faithful recorders of whole rock age and isotopic composition
Accessories in Kaiserstuhl carbonatites and related rocks as accurate and faithful recorders of whole rock age and isotopic composition Open
The accessories perovskite, pyrochlore, zirconolite, calzirtite and melanite from carbonatites and carbonate-rich foidites from the Kaiserstuhl are variously suited for the in situ determination of their U–Pb ages and Sr, Nd- and Hf-isotop…
View article: Oxidation state and metasomatism of the lithospheric mantle beneath the Rae Craton, Canada: strong gradients reflect craton formation and evolution
Oxidation state and metasomatism of the lithospheric mantle beneath the Rae Craton, Canada: strong gradients reflect craton formation and evolution Open
We present the first oxidation state measurements for the subcontinental lithospheric mantle (SCLM) beneath the Rae craton, northern Canada, one of the largest components of the Canadian shield. In combination with major and trace element …
View article: Chemical geodynamics with eclogite - <i>P. Gast Medal Lecture</i>
Chemical geodynamics with eclogite - <i>P. Gast Medal Lecture</i> Open
View article: Breyite inclusions in diamond: experimental evidence for possible dual origin
Breyite inclusions in diamond: experimental evidence for possible dual origin Open
Inclusions of breyite (previously known as walstromite-structured CaSiO3) in diamond are usually interpreted as retrogressed CaSiO3 perovskite trapped in the transition zone or the lower mantle. However, the thermodynamic stability field o…
View article: ROME'S Rise to Power. Geochemical Analysis of Silver Coinage from the Western Mediterranean (Fourth to Second Centuries BCE)
ROME'S Rise to Power. Geochemical Analysis of Silver Coinage from the Western Mediterranean (Fourth to Second Centuries BCE) Open
We present the results of geochemical analysis of silver coinage issued by Rome and dated between the fourth and second century BCE, which are complemented by data of coinage issued by Carthage, the Brettii, and the Greek colony of Emporio…
View article: Retracing Magna Graecia's silver: coupling lead isotopes with a multi‐standard trace element procedure
Retracing Magna Graecia's silver: coupling lead isotopes with a multi‐standard trace element procedure Open
This study presents the results of compositional and lead isotopic analysis of coinage issued by the Greek colonies of Syracuse, Metapontum, Taras and Thurium in the fifth to third centuries bce . The data suggest that each colony in Magna…
View article: Iron oxidation state of mantle minerals determined from L emission spectra by the electron microprobe
Iron oxidation state of mantle minerals determined from L emission spectra by the electron microprobe Open
View article: Oxygen fugacities of the metasomatizing melt in a polymict peridotite from Kimberley
Oxygen fugacities of the metasomatizing melt in a polymict peridotite from Kimberley Open
View article: Redox state of Archean kyanite/corundum eclogites and garnet pyroxenites from Bellsbank, South Africa
Redox state of Archean kyanite/corundum eclogites and garnet pyroxenites from Bellsbank, South Africa Open
View article: Determination of garnet oxidation state using Mössbauer, XANES and the flank method
Determination of garnet oxidation state using Mössbauer, XANES and the flank method Open
View article: Electron microprobe technique for the determination of iron oxidation state in silicate glasses
Electron microprobe technique for the determination of iron oxidation state in silicate glasses Open
We present a new calibration for the determination of the iron oxidation state in silicate glasses by electron probe microanalysis (EPMA) with the "flank method." This method is based on the changes in both intensity and wavelength of the …
View article: Formation of abiotic hydrocarbon from reduction of carbonate in subduction zones: Constraints from petrological observation and experimental simulation
Formation of abiotic hydrocarbon from reduction of carbonate in subduction zones: Constraints from petrological observation and experimental simulation Open
Subduction is a key process for linking the carbon cycle between the Earth's surface and its interior. Knowing the carbonation and decarbonation processes in the subduction zone is essential for understanding the global deep carbon cycle. …
View article: Volatile-rich Metasomatism in the Cratonic Mantle beneath SW Greenland: Link to Kimberlites and Mid-lithospheric Discontinuities
Volatile-rich Metasomatism in the Cratonic Mantle beneath SW Greenland: Link to Kimberlites and Mid-lithospheric Discontinuities Open
The cratonic part of Greenland has been a hotspot of scientific investigation since the discovery of some of the oldest crust on Earth and of significant diamond potential in the underlying lithospheric mantle, the characterization of whic…