1-7 of 7
Subject: Metabasalts
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Journal Article
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Metamorphic Evolution of Kyanite-Bearing Garnet Pyroxenites from the Variscan Orogenic Root: Gföhl Unit, Moldanubian Zone, Austria
Rene Asenbaum and others
Journal of Petrology, Volume 66, Issue 3, March 2025, egaf013, https://doi.org/10.1093/petrology/egaf013
Published: 12 February 2025
Journal Article
Major-Element Geochemistry and Fe3+/ΣFe of Metabasites
Jacob B Forshaw and others
Journal of Petrology, Volume 65, Issue 12, December 2024, egae120, https://doi.org/10.1093/petrology/egae120
Published: 08 November 2024
Journal Article
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Petrology of Tourmaline-Bearing Blueschist from SW Tianshan, China, and Its Implication in B-Rich Fluid Migration in Subduction Zone
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Tingting Shen and others
Journal of Petrology, Volume 65, Issue 11, November 2024, egae116, https://doi.org/10.1093/petrology/egae116
Published: 04 November 2024
Journal Article
Magmatic–Hydrothermal Evolution at the Barren Wushan Pluton, Southeast China: Insight into Controls on Mineralization Potential
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Zhe Chi and others
Journal of Petrology, Volume 65, Issue 5, May 2024, egae047, https://doi.org/10.1093/petrology/egae047
Published: 07 May 2024
Journal Article
Identifying Ultrahigh-Temperature Metamorphism in Basic Granulites
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Bin Wang and Chunjing Wei
Journal of Petrology, Volume 65, Issue 5, May 2024, egae046, https://doi.org/10.1093/petrology/egae046
Published: 06 May 2024
Journal Article
Bridging the Gap in Garnet Diffusion Models at Low Temperatures: Recalibration Using Western Tianshan Eclogitic Breccia
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Junxing Chen and Xu Chu
Journal of Petrology, Volume 65, Issue 3, March 2024, egae012, https://doi.org/10.1093/petrology/egae012
Published: 08 February 2024
Journal Article
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Ultrahigh-Temperature Mafic Granulites in the Rauer Group, East Antarctica: Evidence from Conventional Thermobarometry, Phase Equilibria Modeling, and Rare Earth Element Thermometry
Longyao Chen and others
Journal of Petrology, Volume 64, Issue 4, April 2023, egad014, https://doi.org/10.1093/petrology/egad014
Published: 07 March 2023
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