Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-629-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-629-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Pseudotachylyte as field evidence for lower-crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)
Friedrich Hawemann
CORRESPONDING AUTHOR
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8092 Zürich, Switzerland
Neil S. Mancktelow
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8092 Zürich, Switzerland
Sebastian Wex
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8092 Zürich, Switzerland
Alfredo Camacho
Department of Geological Sciences, University of Manitoba, 125 Dysart Rd, Winnipeg, Manitoba, R3T 2N2, Canada
Giorgio Pennacchioni
Department of Geosciences, University of Padova, Via Gradenigo 6, 35131 Padova, Italy
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28 citations as recorded by crossref.
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- Weak, Seismogenic Faults Inherited From Mesozoic Rifts Control Mountain Building in the Andean Foreland S. Wimpenny 10.1029/2021GC010270
- 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. 10.1016/j.tecto.2018.10.024
- Inverted distribution of ductile deformation in the relatively “dry” middle crust across the Woodroffe Thrust, central Australia S. Wex et al. 10.5194/se-9-859-2018
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- New perspectives on ‘geological strain rates’ calculated from both naturally deformed and actively deforming rocks Å. Fagereng & J. Biggs 10.1016/j.jsg.2018.10.004
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- Transient Brittle‐Ductile Transition Depth Induced by Moderate‐Large Earthquakes in Southern and Baja California Y. Cheng & Y. Ben‐Zion 10.1029/2019GL084315
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- 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. 10.1098/rsta.2019.0416
- Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway K. Dunkel et al. 10.1098/rsta.2019.0423
- Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia) F. Hawemann et al. 10.1029/2018JB016559
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- 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. 10.1016/j.tecto.2021.229185
- Dynamic Evolution of Porosity in Lower‐Crustal Faults During the Earthquake Cycle S. Michalchuk et al. 10.1029/2023JB026809
- High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway K. Dunkel et al. 10.1130/G48002.1
- Dating fossil lower-crustal earthquakes by in-situ apatite U-Pb geochronology S. Zertani et al. 10.1016/j.epsl.2024.118621
- Pseudotachylytes in felsic lower-crustal rocks of the Calabrian Serre massif: A record of deep- or shallow-crustal earthquakes? S. Papa et al. 10.1016/j.lithos.2023.107375
- 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. 10.1017/S0016756819000062
- Time‐Lapse Record of an Earthquake in the Dry Felsic Lower Continental Crust Preserved in a Pseudotachylyte‐Bearing Fault N. Mancktelow et al. 10.1029/2021JB022878
- Earthquake-induced transformation of the lower crust B. Jamtveit et al. 10.1038/s41586-018-0045-y
27 citations as recorded by crossref.
- Strain hardening induced by crystal plasticity: A new mechanism for brittle failure in garnets R. Dubosq et al. 10.1016/j.epsl.2023.118273
- Transient High Strain Rate During Localized Viscous Creep in the Dry Lower Continental Crust (Lofoten, Norway) L. Campbell & L. Menegon 10.1029/2019JB018052
- Weak, Seismogenic Faults Inherited From Mesozoic Rifts Control Mountain Building in the Andean Foreland S. Wimpenny 10.1029/2021GC010270
- 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. 10.1016/j.tecto.2018.10.024
- Inverted distribution of ductile deformation in the relatively “dry” middle crust across the Woodroffe Thrust, central Australia S. Wex et al. 10.5194/se-9-859-2018
- Infiltration of volatile-rich mafic melt in lower crustal peridotites provokes lower crustal earthquakes E. Ryan et al. 10.1016/j.jsg.2022.104708
- Metamorphic geology: progress and perspectives P. Lanari et al. 10.1144/SP478-2018-186
- The Effects of Earthquakes and Fluids on the Metamorphism of the Lower Continental Crust B. Jamtveit et al. 10.1029/2018JB016461
- Source mechanism of a lower crust earthquake beneath the Himalayas and its possible relation to metamorphism C. Alvizuri & G. Hetényi 10.1016/j.tecto.2019.06.023
- New perspectives on ‘geological strain rates’ calculated from both naturally deformed and actively deforming rocks Å. Fagereng & J. Biggs 10.1016/j.jsg.2018.10.004
- Rheology Dependent on the Distance to the Propagating Thrust Tip—(Ultra‐)Mylonites and Pseudotachylytes of the Silvretta Basal Thrust L. Brückner et al. 10.1029/2023TC008010
- Fracturing and crystal plastic behaviour of garnet under seismic stress in the dry lower continental crust (Musgrave Ranges, Central Australia) F. Hawemann et al. 10.5194/se-10-1635-2019
- Transient Brittle‐Ductile Transition Depth Induced by Moderate‐Large Earthquakes in Southern and Baja California Y. Cheng & Y. Ben‐Zion 10.1029/2019GL084315
- 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. 10.1111/jmg.12646
- 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. 10.1029/2020GC009028
- 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. 10.1098/rsta.2019.0416
- Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway K. Dunkel et al. 10.1098/rsta.2019.0423
- Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia) F. Hawemann et al. 10.1029/2018JB016559
- Record of intermediate-depth subduction seismicity in a dry slab from an exhumed ophiolite G. Pennacchioni et al. 10.1016/j.epsl.2020.116490
- Rheological evolution of a pseudotachylyte-bearing deep crustal shear zone in the western Canadian shield O. Orlandini & K. Mahan 10.1016/j.jsg.2020.104188
- 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. 10.1016/j.tecto.2021.229185
- Dynamic Evolution of Porosity in Lower‐Crustal Faults During the Earthquake Cycle S. Michalchuk et al. 10.1029/2023JB026809
- High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway K. Dunkel et al. 10.1130/G48002.1
- Dating fossil lower-crustal earthquakes by in-situ apatite U-Pb geochronology S. Zertani et al. 10.1016/j.epsl.2024.118621
- Pseudotachylytes in felsic lower-crustal rocks of the Calabrian Serre massif: A record of deep- or shallow-crustal earthquakes? S. Papa et al. 10.1016/j.lithos.2023.107375
- 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. 10.1017/S0016756819000062
- Time‐Lapse Record of an Earthquake in the Dry Felsic Lower Continental Crust Preserved in a Pseudotachylyte‐Bearing Fault N. Mancktelow et al. 10.1029/2021JB022878
1 citations as recorded by crossref.
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Latest update: 21 Nov 2024