28 citations as recorded by crossref.

1. Strain hardening induced by crystal plasticity: A new mechanism for brittle failure in garnets R. Dubosq et al.
2. Transient High Strain Rate During Localized Viscous Creep in the Dry Lower Continental Crust (Lofoten, Norway) L. Campbell & L. Menegon
3. Weak, Seismogenic Faults Inherited From Mesozoic Rifts Control Mountain Building in the Andean Foreland S. Wimpenny
4. Interplay between seismic fracture and aseismic creep in the Woodroffe Thrust, central Australia – Inferences for the rheology of relatively dry continental mid-crustal levels S. Wex et al.
5. Inverted distribution of ductile deformation in the relatively “dry” middle crust across the Woodroffe Thrust, central Australia S. Wex et al.
6. Infiltration of volatile-rich mafic melt in lower crustal peridotites provokes lower crustal earthquakes E. Ryan et al.
7. Metamorphic geology: progress and perspectives P. Lanari et al.
8. The Effects of Earthquakes and Fluids on the Metamorphism of the Lower Continental Crust B. Jamtveit et al.
9. Source mechanism of a lower crust earthquake beneath the Himalayas and its possible relation to metamorphism C. Alvizuri & G. Hetényi
10. New perspectives on ‘geological strain rates’ calculated from both naturally deformed and actively deforming rocks Å. Fagereng & J. Biggs
11. Rheology Dependent on the Distance to the Propagating Thrust Tip—(Ultra‐)Mylonites and Pseudotachylytes of the Silvretta Basal Thrust L. Brückner et al.
12. Fracturing and crystal plastic behaviour of garnet under seismic stress in the dry lower continental crust (Musgrave Ranges, Central Australia) F. Hawemann et al.
13. Transient Brittle‐Ductile Transition Depth Induced by Moderate‐Large Earthquakes in Southern and Baja California Y. Cheng & Y. Ben‐Zion
14. A window into an older orogenic cycle: P–T conditions and timing of the pre‐Alpine history of the Dora‐Maira Massif (Western Alps) F. Nosenzo et al.
15. Evolution of Brittle Structures in Plagioclase‐Rich Rocks at High‐Pressure and High‐Temperature Conditions—Linking Laboratory Results to Field Observations S. Incel et al.
16. The earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway) L. Menegon et al.
17. Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway K. Dunkel et al.
18. Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia) F. Hawemann et al.
19. Record of intermediate-depth subduction seismicity in a dry slab from an exhumed ophiolite G. Pennacchioni et al.
20. Rheological evolution of a pseudotachylyte-bearing deep crustal shear zone in the western Canadian shield O. Orlandini & K. Mahan
21. Residual stress in diopside: insight into localized transient high stress in seismogenic faults in the lower crust, Lofoten, Norway H. van Schrojenstein Lantman et al.
22. The pseudotachylytes at the base of the Silvretta Nappe: A newly discovered recent generation and the tectonomometamophic evolution of the Nappe L. Pittarello et al.
23. Dynamic Evolution of Porosity in Lower‐Crustal Faults During the Earthquake Cycle S. Michalchuk et al.
24. High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway K. Dunkel et al.
25. Dating fossil lower-crustal earthquakes by in-situ apatite U-Pb geochronology S. Zertani et al.
26. Pseudotachylytes in felsic lower-crustal rocks of the Calabrian Serre massif: A record of deep- or shallow-crustal earthquakes? S. Papa et al.
27. Fault rocks within the blueschist metabasalts of the Diamante–Terranova unit (southern Italy): potential fossil record of intermediate-depth subduction earthquakes S. Vitale et al.
28. Time‐Lapse Record of an Earthquake in the Dry Felsic Lower Continental Crust Preserved in a Pseudotachylyte‐Bearing Fault N. Mancktelow et al.