13 citations as recorded by crossref.

1. Temperature, fluid content and rheology of localized ductile shear zones in subsolidus cooling plutons A. Ceccato et al. 10.1111/jmg.12553
2. 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
3. Exceptional Scarp Preservation in SW Namibia Reveals Geological Controls on Large Magnitude Intraplate Seismicity in Southern Africa R. Muir et al. 10.1029/2022TC007693
4. 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
5. 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
6. The strength of earthquake-generating faults A. Copley 10.1144/jgs2017-037
7. Weaker Than Weakest: On the Strength of Shear Zones C. Stenvall et al. 10.1029/2019GL083388
8. Geochemical evolution of magmatic rocks in the Vioolsdrif Domain, Namibia R. Minnitt & K. Esbensen 10.25131/sajg.126.0001
9. 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
10. 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
11. 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
12. 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
13. 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