Articles | Volume 7, issue 5
https://doi.org/10.5194/se-7-1331-2016
© Author(s) 2016. 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-7-1331-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Mid-crustal shear zone development under retrograde conditions: pressure–temperature–fluid constraints from the Kuckaus Mylonite Zone, Namibia
Johann F. A. Diener
CORRESPONDING AUTHOR
Department of Geological Sciences, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa
Åke Fagereng
Department of Geological Sciences, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa
present address: School of Earth & Ocean Sciences, Cardiff University, Cardiff CF10 3AT, UK
Sukey A. J. Thomas
Department of Geological Sciences, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa
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Cited
14 citations as recorded by crossref.
- Temperature, fluid content and rheology of localized ductile shear zones in subsolidus cooling plutons A. Ceccato et al. 10.1111/jmg.12553
- Role of myrmekite and associated deformation fabrics in controlling development of granitic mylonites in the Pofadder Shear Zone of southern Namibia D. Cisneros-Lazaro et al. 10.1007/s00410-019-1555-9
- Exceptional Scarp Preservation in SW Namibia Reveals Geological Controls on Large Magnitude Intraplate Seismicity in Southern Africa R. Muir et al. 10.1029/2022TC007693
- Low‐Temperature Frictional Characteristics of Chlorite‐Epidote‐Amphibole Assemblages: Implications for Strength and Seismic Style of Retrograde Fault Zones Å. Fagereng & M. Ikari 10.1029/2020JB019487
- Rate-and-state friction of epidote gouge under hydrothermal conditions and implications for the stability of subducting faults under greenschist metamorphic conditions M. An et al. 10.1016/j.tecto.2024.230497
- The strength of earthquake-generating faults A. Copley 10.1144/jgs2017-037
- Weaker Than Weakest: On the Strength of Shear Zones C. Stenvall et al. 10.1029/2019GL083388
- Deformation by Pressure Solution and Grain Boundary Sliding in a Retrograde Shear Zone in Southern New England, USA R. Wintsch et al. 10.2475/001c.125064
- Geochemical evolution of magmatic rocks in the Vioolsdrif Domain, Namibia R. Minnitt & K. Esbensen 10.25131/sajg.126.0001
- Partial melting and strain localization in metapelites at very low-pressure conditions: The northern Apennines magmatic arc on the Island of Elba, Italy S. Papeschi et al. 10.1016/j.lithos.2019.105230
- On the petrology and microstructures of small-scale ductile shear zones in granitoid rocks: An overview A. Ceccato et al. 10.1016/j.jsg.2022.104667
- Sources and Effects of Fluids in Continental Retrograde Shear Zones: Insights from the Kuckaus Mylonite Zone, Namibia C. Stenvall et al. 10.1155/2020/3023268
- Paleoproterozoic amphibolite facies retrogression and exhumation of Archean metapelitic granulites in the Southern Marginal Zone of the Limpopo Belt, South Africa N. Madlakana et al. 10.1016/j.precamres.2019.105532
- Assessing the importance of H2O content in the tectono‐metamorphic evolution of shear zones: A case study from the Dora‐Maira Massif (Western Alps) S. Nerone et al. 10.1111/jmg.12750
14 citations as recorded by crossref.
- Temperature, fluid content and rheology of localized ductile shear zones in subsolidus cooling plutons A. Ceccato et al. 10.1111/jmg.12553
- Role of myrmekite and associated deformation fabrics in controlling development of granitic mylonites in the Pofadder Shear Zone of southern Namibia D. Cisneros-Lazaro et al. 10.1007/s00410-019-1555-9
- Exceptional Scarp Preservation in SW Namibia Reveals Geological Controls on Large Magnitude Intraplate Seismicity in Southern Africa R. Muir et al. 10.1029/2022TC007693
- Low‐Temperature Frictional Characteristics of Chlorite‐Epidote‐Amphibole Assemblages: Implications for Strength and Seismic Style of Retrograde Fault Zones Å. Fagereng & M. Ikari 10.1029/2020JB019487
- Rate-and-state friction of epidote gouge under hydrothermal conditions and implications for the stability of subducting faults under greenschist metamorphic conditions M. An et al. 10.1016/j.tecto.2024.230497
- The strength of earthquake-generating faults A. Copley 10.1144/jgs2017-037
- Weaker Than Weakest: On the Strength of Shear Zones C. Stenvall et al. 10.1029/2019GL083388
- Deformation by Pressure Solution and Grain Boundary Sliding in a Retrograde Shear Zone in Southern New England, USA R. Wintsch et al. 10.2475/001c.125064
- Geochemical evolution of magmatic rocks in the Vioolsdrif Domain, Namibia R. Minnitt & K. Esbensen 10.25131/sajg.126.0001
- Partial melting and strain localization in metapelites at very low-pressure conditions: The northern Apennines magmatic arc on the Island of Elba, Italy S. Papeschi et al. 10.1016/j.lithos.2019.105230
- On the petrology and microstructures of small-scale ductile shear zones in granitoid rocks: An overview A. Ceccato et al. 10.1016/j.jsg.2022.104667
- Sources and Effects of Fluids in Continental Retrograde Shear Zones: Insights from the Kuckaus Mylonite Zone, Namibia C. Stenvall et al. 10.1155/2020/3023268
- Paleoproterozoic amphibolite facies retrogression and exhumation of Archean metapelitic granulites in the Southern Marginal Zone of the Limpopo Belt, South Africa N. Madlakana et al. 10.1016/j.precamres.2019.105532
- Assessing the importance of H2O content in the tectono‐metamorphic evolution of shear zones: A case study from the Dora‐Maira Massif (Western Alps) S. Nerone et al. 10.1111/jmg.12750
Discussed (final revised paper)
Latest update: 14 Dec 2024