Works matching AU Höfer, Heidi
Results: 17
High-Pressure Synthesis of Tantalum Nitride Having Orthorhombic U<sub>2</sub>S<sub>3</sub> Structure.
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- Advanced Functional Materials, 2009, v. 19, n. 14, p. 2282, doi. 10.1002/adfm.200801923
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The influence of Fe on garnet-orthopyroxene and garnet-olivine geothermometers.
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- Contributions to Mineralogy & Petrology, 2014, v. 167, n. 2, p. 1, doi. 10.1007/s00410-014-0972-z
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Oxidation of the Kaapvaal lithospheric mantle driven by metasomatism.
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- Contributions to Mineralogy & Petrology, 2009, v. 157, n. 4, p. 491, doi. 10.1007/s00410-008-0348-3
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High-pressure synthesis of priderite and members of the lindsleyite-mathiasite and hawthorneite-yimengite series.
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- Contributions to Mineralogy & Petrology, 1994, v. 117, n. 2, p. 164, doi. 10.1007/BF00286840
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Accessories in Kaiserstuhl carbonatites and related rocks as accurate and faithful recorders of whole rock age and isotopic composition.
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- International Journal of Earth Sciences, 2022, v. 111, n. 2, p. 573, doi. 10.1007/s00531-021-02130-9
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Metasomatism and oxidation state of the lithospheric mantle beneath the Rae craton, Canada as revealed by xenoliths from Somerset Island and Pelly Bay.
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- Geophysical Research Abstracts, 2019, v. 21, p. 1
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Ferropericlase crystallization under upper mantle conditions: implications for inclusions in diamond.
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- Geophysical Research Abstracts, 2019, v. 21, p. 1
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Mélange Signatures and Low Oxygen Fugacity in Eclogite Xenoliths From the Crust‐Mantle Transition Below a Mesoproterozoic Collision Belt.
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- Journal of Geophysical Research. Solid Earth, 2024, v. 129, n. 2, p. 1, doi. 10.1029/2023JB027894
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Ferropericlase inclusions in ultradeep diamonds from Sao Luiz (Brazil): high Li abundances and diverse Li-isotope and trace element compositions suggest an origin from a subduction mélange.
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- Mineralogy & Petrology, 2018, v. 112, p. 291, doi. 10.1007/s00710-018-0572-0
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A fast open data reduction workflow for the electron microprobe flank method to determine Fe<sup>3+</sup>/ΣFe contents in minerals.
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- American Mineralogist, 2024, v. 109, n. 8, p. 1387, doi. 10.2138/am-2023-9122
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Ferric-ferrous iron ratios of experimental majoritic garnet and clinopyroxene as a function of oxygen fugacity.
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- American Mineralogist, 2020, v. 105, n. 12, p. 1866, doi. 10.2138/am-2020-7265
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Electron microprobe technique for the determination of iron oxidation state in silicate glasses.
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- American Mineralogist, 2018, v. 103, n. 9, p. 1445, doi. 10.2138/am-2018-6437
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High-Mg and Low-Mg Mantle Eclogites from Koidu (West African Craton) Linked by Neoproterozoic Ultramafic Melt Metasomatism of Subducted Archaean Plateau-like Oceanic Crust.
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- Journal of Petrology, 2019, v. 60, n. 4, p. 723, doi. 10.1093/petrology/egz011
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Element Transfer and Redox Conditions in Continental Subduction Zones: New Insights from Peridotites of the Ulten Zone, North Italy.
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- Journal of Petrology, 2019, v. 60, n. 2, p. 231, doi. 10.1093/petrology/egy112
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A Reconnaissance Study of Ti-minerals in Cratonic Granulite Xenoliths and their Potential as Recorders of Lower Crust Formation and Evolution.
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- Journal of Petrology, 2017, v. 58, n. 10, p. 2007, doi. 10.1093/petrology/egx080
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Oxidation state and metasomatism of the lithospheric mantle beneath the Rae Craton, Canada: strong gradients reflect craton formation and evolution.
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- Scientific Reports, 2021, v. 11, n. 1, p. 1, doi. 10.1038/s41598-021-83261-6
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Breyite inclusions in diamond: experimental evidence for possible dual origin.
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- European Journal of Minerology, 2020, v. 32, n. 1, p. 171, doi. 10.5194/ejm-32-171-2020
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