Articles | Volume 8, issue 1
https://doi.org/10.5194/se-8-93-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-8-93-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Review article
| 
06 Feb 2017
Review article |
| 06 Feb 2017
Arrested development – a comparative analysis of multilayer corona textures in high-grade metamorphic rocks
Paula Ogilvie
School of Geosciences, University of the Witwatersrand, P O WITS, Johannesburg 2050, South Africa
Roger L. Gibson
CORRESPONDING AUTHOR
School of Geosciences, University of the Witwatersrand, P O WITS, Johannesburg 2050, South Africa
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Cited
14 citations as recorded by crossref.
- Ultra-fast metamorphic reaction during regional metamorphism J. Liu et al. 10.1016/j.gca.2025.01.036
- Corona-Type Textures in Ultrabasic Complexes of the Serpentinite Belt, Kola Peninsula, Russia A. Barkov et al. 10.3390/min13010115
- Controls on the scales of equilibrium during granulite facies metamorphism R. Mitchell et al. 10.1111/jmg.12579
- Comment on “Neoarchean arc magmatism and Paleoproterozoic high-pressure granulite-facies metamorphism in the southern Motloutse Complex, eastern Botswana: Implications for the western extension of the Limpopo Complex” D. Mfa et al. 10.1016/j.precamres.2022.106729
- А History of Coronitic Metagabbronorites in the Belomorian Province, Fennoscandian Shield: U-Pb (CA-ID-TIMS) Dating of Zircon–Baddeleyite Aggregates E. Salnikova et al. 10.1134/S0869591122060066
- Origin of multilayer corona textures in mafic granulites from the Sandmata Complex, Aravalli Craton (northwestern India): petrological characteristics and tectonic implications S. Ghosh et al. 10.1007/s00410-021-01782-9
- Competing Roles of Evolving P–T Conditions, Equilibration Volume and Chemical Potential Landscape in the Formation of Corona Texture: a Case Study from the Southern Granulite Terrane, India A. Dey et al. 10.1093/petrology/egad083
- Paleoproterozoic ultrahigh‐temperature mafic granulites with a high‐pressure prograde path from the Alxa Block: Implications on the tectonic evolution of the Khondalite Belt, North China Craton L. Zou et al. 10.1111/jmg.12764
- Late Triassic ultrahigh-temperature mafic granulite from the North Dabie terrane, Central China H. Lei et al. 10.1016/j.lithos.2025.108165
- Genesis of coronae and implications of an early Neoproterozoic thermal event: a case study from SE Chotanagpur Granite Gneissic Complex, India V. Adak & U. Dutta 10.1017/S0016756820000357
- Three Types of Mantle Eclogite from Two Layers of Oceanic Crust: A Key Case of Metasomatically-Aided Transformation of Low-to-High-Magnesian Eclogite N. Korolev et al. 10.1093/petrology/egab070
- Reply to ‘Comment on “Neoarchean arc magmatism and Paleoproterozoic high-pressure granulite-facies metamorphism in the southern Motloutse Complex, eastern Botswana: Implication for the western extension of the Limpopo Complex”’ by Mfa et al. T. Basupi et al. 10.1016/j.precamres.2022.106730
- A Quantitative Approach to the Analysis of Reactive Mineralogy and Surface Area L. Anovitz et al. 10.1021/acsearthspacechem.1c00198
- Dating corona formation in high-grade rocks: integrated garnet and zircon petrochronology of granulite-facies rocks in the North China Craton K. Du et al. 10.1007/s00410-023-02077-x
14 citations as recorded by crossref.
- Ultra-fast metamorphic reaction during regional metamorphism J. Liu et al. 10.1016/j.gca.2025.01.036
- Corona-Type Textures in Ultrabasic Complexes of the Serpentinite Belt, Kola Peninsula, Russia A. Barkov et al. 10.3390/min13010115
- Controls on the scales of equilibrium during granulite facies metamorphism R. Mitchell et al. 10.1111/jmg.12579
- Comment on “Neoarchean arc magmatism and Paleoproterozoic high-pressure granulite-facies metamorphism in the southern Motloutse Complex, eastern Botswana: Implications for the western extension of the Limpopo Complex” D. Mfa et al. 10.1016/j.precamres.2022.106729
- А History of Coronitic Metagabbronorites in the Belomorian Province, Fennoscandian Shield: U-Pb (CA-ID-TIMS) Dating of Zircon–Baddeleyite Aggregates E. Salnikova et al. 10.1134/S0869591122060066
- Origin of multilayer corona textures in mafic granulites from the Sandmata Complex, Aravalli Craton (northwestern India): petrological characteristics and tectonic implications S. Ghosh et al. 10.1007/s00410-021-01782-9
- Competing Roles of Evolving P–T Conditions, Equilibration Volume and Chemical Potential Landscape in the Formation of Corona Texture: a Case Study from the Southern Granulite Terrane, India A. Dey et al. 10.1093/petrology/egad083
- Paleoproterozoic ultrahigh‐temperature mafic granulites with a high‐pressure prograde path from the Alxa Block: Implications on the tectonic evolution of the Khondalite Belt, North China Craton L. Zou et al. 10.1111/jmg.12764
- Late Triassic ultrahigh-temperature mafic granulite from the North Dabie terrane, Central China H. Lei et al. 10.1016/j.lithos.2025.108165
- Genesis of coronae and implications of an early Neoproterozoic thermal event: a case study from SE Chotanagpur Granite Gneissic Complex, India V. Adak & U. Dutta 10.1017/S0016756820000357
- Three Types of Mantle Eclogite from Two Layers of Oceanic Crust: A Key Case of Metasomatically-Aided Transformation of Low-to-High-Magnesian Eclogite N. Korolev et al. 10.1093/petrology/egab070
- Reply to ‘Comment on “Neoarchean arc magmatism and Paleoproterozoic high-pressure granulite-facies metamorphism in the southern Motloutse Complex, eastern Botswana: Implication for the western extension of the Limpopo Complex”’ by Mfa et al. T. Basupi et al. 10.1016/j.precamres.2022.106730
- A Quantitative Approach to the Analysis of Reactive Mineralogy and Surface Area L. Anovitz et al. 10.1021/acsearthspacechem.1c00198
- Dating corona formation in high-grade rocks: integrated garnet and zircon petrochronology of granulite-facies rocks in the North China Craton K. Du et al. 10.1007/s00410-023-02077-x
Discussed (final revised paper)
Latest update: 08 Jul 2025
Short summary
Coronas are vital clues to the presence of arrested reaction in metamorphic rocks. We review formation mechanisms of coronas and approaches utilized to model their evolution in P–T–X space. Forward modelling employing calculated chemical potential gradients allows a far more nuanced understanding of the intricacies that govern metamorphic reaction. These models have critical implications for the limitations and opportunities coronas afford in interpreting the evolution of metamorphic terranes.
Coronas are vital clues to the presence of arrested reaction in metamorphic rocks. We review...
