Experimental mineralogy, petrology, and geochemistry
Experimental mineralogy, petrology, and geochemistry
This collection is designed to emphasize the significance of experimental mineralogy, petrology, and geochemistry in the fields of geoscience and planetary science. All types of experimental set-ups and experimental approaches are welcome. Topics of interest include planetary processes, deep Earth, mantle petrology, fluid–rock interaction, melt–rock interaction, melt properties, rock deformation, ore formation, magmatic and metamorphic petrology, mineral physics, bio-mineralogy, and methodological developments. This list is not exhaustive.

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09 Jan 2026
Spaltiite, Tl2Cu2As2S5, one more new thallium sulfosalt mineral from Lengenbach quarry, Binn, Switzerland
Stefan Graeser, Dan Topa, Herta Silvia Effenberger, Emil Makovicky, Werner Hermann Paar, and George Dincă
Eur. J. Mineral., 38, 27–37, https://doi.org/10.5194/ejm-38-27-2026,https://doi.org/10.5194/ejm-38-27-2026, 2026
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07 Jan 2026
Trace element distribution between rhyolitic melts and minerals in highly crystalline assemblages: experimental approach using a quartz trap
Francesco Vetere, Kristina Schimetzek, Maurizio Petrelli, Fleurice Parat, André Stechern, Christian Singer, and Francois Holtz
Eur. J. Mineral., 38, 9–25, https://doi.org/10.5194/ejm-38-9-2026,https://doi.org/10.5194/ejm-38-9-2026, 2026
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16 Dec 2025
Analyzing trace element distribution and purification of vein quartz: a case study of Qianqi Furong mine in Inner Mongolia
Shaoyiqing Qu, Xiaoyong Yang, Mei Xia, Zhenhui Hou, and Yicun Wang
Eur. J. Mineral., 37, 953–970, https://doi.org/10.5194/ejm-37-953-2025,https://doi.org/10.5194/ejm-37-953-2025, 2025
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25 Nov 2025
Ordering of tetrahedral and octahedral layers in synthetic lepidolites and Li-muscovites: two-dimensional {1H} → 29Si ∕ 27Al CPMAS HETCOR and {19F} → 29Si ∕ 27Al CPMAS HETCOR spectroscopy
Michael Fechtelkord and Lara Sulcek
Eur. J. Mineral., 37, 877–888, https://doi.org/10.5194/ejm-37-877-2025,https://doi.org/10.5194/ejm-37-877-2025, 2025
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