Articles | Volume 8, issue 1
https://doi.org/10.5194/se-8-199-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-8-199-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Feb 2017
Research article |
| 21 Feb 2017
Rheological transitions in the middle crust: insights from Cordilleran metamorphic core complexes
Frances J. Cooper
CORRESPONDING AUTHOR
School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK
John P. Platt
Department of Earth Sciences, University of Southern California, Los
Angeles, CA 90089, USA
Whitney M. Behr
School of Geological Sciences, Jackson School of Geosciences,
University of Texas at Austin, Austin, TX 78712, USA
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Cited
21 citations as recorded by crossref.
- Impact of Moisture Content on the Brittle-Ductile Transition and Microstructure of Sandstone under Dynamic Loading Conditions A. Lu et al. 10.1155/2021/6690171
- Using Syntectonic Calcite Veins to Reconstruct the Strength Evolution of an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea M. Mizera et al. 10.1029/2021JB021916
- What controls the width of ductile shear zones? T. Cawood & J. Platt 10.1016/j.tecto.2021.229033
- Recent advances in petrochronology: from dates to ages and rates of deep orogenic processes L. Labrousse et al. 10.5802/crgeos.234
- Slow‐to‐Fast Deformation in Mafic Fault Rocks on an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea M. Mizera et al. 10.1029/2020GC009171
- Compressional metamorphic core complexes, low-angle normal faults and extensional fabrics in compressional tectonic settings M. Searle & T. Lamont 10.1017/S0016756819000207
- Deformation conditions during syn-convergent extension along the Cordillera Blanca shear zone, Peru C. Hughes et al. 10.1130/GES02040.1
- Shear zone evolution during core complex exhumation – Implications for continental detachments J. Wiest et al. 10.1016/j.jsg.2020.104139
- The fold illusion: The origins and implications of ogives on silicic lavas G. Andrews et al. 10.1016/j.epsl.2020.116643
- 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
- Deformation conditions and kinematic vorticity within the footwall shear zone of the Wildhorse detachment system, Pioneer metamorphic core complex, Idaho R. McFadden et al. 10.1016/j.jsg.2023.105031
- Research on Brittleness Characteristic Coefficient of Thermal Damage Rock Based on Postpeak Stage of Stress‐Strain Curve J. Liu & A. Thirumurugan 10.1155/2024/3790073
- Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite T. Cawood & J. Platt 10.1029/2020GC009384
- Evolution of a rapidly slipping, active low-angle normal fault, Suckling-Dayman metamorphic core complex, SE Papua New Guinea T. Little et al. 10.1130/B35051.1
- Brittle and ductile deformation in extensional tectonic settings within the Central Asian Orogenic Belt (evidence from Geotransect ṢEast Siberian Plate ‐ Siberian Craton –Central Asian Beltṣ) I. Kudriavtcev et al. 10.1111/1755-6724.13975
- A Middle Crustal Channel of Radial Anisotropy Beneath the Northeastern Basin and Range J. Wilgus et al. 10.1029/2020TC006140
- Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
- Linked microstructural and geochemical evolution of mylonitic quartzite during exhumation of a core complex J. Taylor et al. 10.1016/j.jsg.2023.104846
- Fault reactivation and strain partitioning across the brittle-ductile transition G. Meyer et al. 10.1130/G46516.1
- Deep Crustal Flow Within Postorogenic Metamorphic Core Complexes: Insights From the Southern Western Gneiss Region of Norway J. Wiest et al. 10.1029/2019TC005708
- Thermo-kinematic modeling of detachment-dominated extension, northeastern Death Valley area, USA: Implications for mid-crustal thermal-rheological evolution B. Lutz et al. 10.1016/j.tecto.2021.228755
21 citations as recorded by crossref.
- Impact of Moisture Content on the Brittle-Ductile Transition and Microstructure of Sandstone under Dynamic Loading Conditions A. Lu et al. 10.1155/2021/6690171
- Using Syntectonic Calcite Veins to Reconstruct the Strength Evolution of an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea M. Mizera et al. 10.1029/2021JB021916
- What controls the width of ductile shear zones? T. Cawood & J. Platt 10.1016/j.tecto.2021.229033
- Recent advances in petrochronology: from dates to ages and rates of deep orogenic processes L. Labrousse et al. 10.5802/crgeos.234
- Slow‐to‐Fast Deformation in Mafic Fault Rocks on an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea M. Mizera et al. 10.1029/2020GC009171
- Compressional metamorphic core complexes, low-angle normal faults and extensional fabrics in compressional tectonic settings M. Searle & T. Lamont 10.1017/S0016756819000207
- Deformation conditions during syn-convergent extension along the Cordillera Blanca shear zone, Peru C. Hughes et al. 10.1130/GES02040.1
- Shear zone evolution during core complex exhumation – Implications for continental detachments J. Wiest et al. 10.1016/j.jsg.2020.104139
- The fold illusion: The origins and implications of ogives on silicic lavas G. Andrews et al. 10.1016/j.epsl.2020.116643
- 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
- Deformation conditions and kinematic vorticity within the footwall shear zone of the Wildhorse detachment system, Pioneer metamorphic core complex, Idaho R. McFadden et al. 10.1016/j.jsg.2023.105031
- Research on Brittleness Characteristic Coefficient of Thermal Damage Rock Based on Postpeak Stage of Stress‐Strain Curve J. Liu & A. Thirumurugan 10.1155/2024/3790073
- Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite T. Cawood & J. Platt 10.1029/2020GC009384
- Evolution of a rapidly slipping, active low-angle normal fault, Suckling-Dayman metamorphic core complex, SE Papua New Guinea T. Little et al. 10.1130/B35051.1
- Brittle and ductile deformation in extensional tectonic settings within the Central Asian Orogenic Belt (evidence from Geotransect ṢEast Siberian Plate ‐ Siberian Craton –Central Asian Beltṣ) I. Kudriavtcev et al. 10.1111/1755-6724.13975
- A Middle Crustal Channel of Radial Anisotropy Beneath the Northeastern Basin and Range J. Wilgus et al. 10.1029/2020TC006140
- Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
- Linked microstructural and geochemical evolution of mylonitic quartzite during exhumation of a core complex J. Taylor et al. 10.1016/j.jsg.2023.104846
- Fault reactivation and strain partitioning across the brittle-ductile transition G. Meyer et al. 10.1130/G46516.1
- Deep Crustal Flow Within Postorogenic Metamorphic Core Complexes: Insights From the Southern Western Gneiss Region of Norway J. Wiest et al. 10.1029/2019TC005708
- Thermo-kinematic modeling of detachment-dominated extension, northeastern Death Valley area, USA: Implications for mid-crustal thermal-rheological evolution B. Lutz et al. 10.1016/j.tecto.2021.228755
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Short summary
We examine how deformation of the Earth’s crust varies with depth beneath the surface. By looking in detail at exhumed rocks from three case studies in the USA, we identify three main deformation zones: 1, a brittle deformation zone (low temperatures mean rocks break along faults and fractures); 2, a localized deformation zone (warmer rocks deform along discrete zones that shear but do not break); and 3, a distributed deformation zone (hot rocks flow ductilely and no discrete shearing occurs).
We examine how deformation of the Earth’s crust varies with depth beneath the surface. By...
