Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1025-2019
© Author(s) 2019. 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-10-1025-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Jul 2019
Research article |
| 04 Jul 2019
| 04 Jul 2019
The internal structure and composition of a plate-boundary-scale serpentinite shear zone: the Livingstone Fault, New Zealand
Matthew S. Tarling
CORRESPONDING AUTHOR
Department of Geology, University of Otago, 360 Leith Street, 9016 Dunedin, New Zealand
Steven A. F. Smith
Department of Geology, University of Otago, 360 Leith Street, 9016 Dunedin, New Zealand
James M. Scott
Department of Geology, University of Otago, 360 Leith Street, 9016 Dunedin, New Zealand
Jeremy S. Rooney
Department of Chemistry, University of Otago, Union Place West, 9016 Dunedin, New Zealand
Cecilia Viti
Dipartimento di Scienze Fisiche, della Terra e dell'Ambiente, Università degli Studi di Siena, Siena, Italy
Keith C. Gordon
Department of Chemistry, University of Otago, Union Place West, 9016 Dunedin, New Zealand
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Cited
19 citations as recorded by crossref.
- Element and Sr–O isotope redistribution across a plate boundary-scale crustal serpentinite mélange shear zone, and implications for the slab-mantle interface J. Scott et al. 10.1016/j.epsl.2019.06.034
- Crystallographic orientation mapping of lizardite serpentinite by Raman spectroscopy M. Tarling et al. 10.5194/ejm-34-285-2022
- Evolution of a Normal Fault System Along Eastern Gondwana, New Zealand T. Sahoo et al. 10.1029/2020TC006181
- Heterogeneity in Microseismicity and Stress Near Rupture‐Limiting Section Boundaries Along the Late‐Interseismic Alpine Fault E. Warren‐Smith et al. 10.1029/2022JB025219
- Fluid overpressure from chemical reactions in serpentinite within the source region of deep episodic tremor M. Tarling et al. 10.1038/s41561-019-0470-z
- The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling T. Phillips et al. 10.5194/se-14-369-2023
- Rheology of Naturally Deformed Antigorite Serpentinite: Strain and Strain‐Rate Dependence at Mantle‐Wedge Conditions C. Tulley et al. 10.1029/2022GL098945
- Slip and stress in block-in-matrix shear zones: 1. microstructure and mineralogy of a serpentine-filled dilational jog S. Smith et al. 10.1016/j.jsg.2024.105220
- Geological fingerprints of deep slow earthquakes: A review of field constraints and directions for future research J. Platt et al. 10.1130/GES02722.1
- Si- versus Mg-metasomatism at the crust–mantle interface: insights from experiments, natural observations and geochemical modeling A. Okamoto & R. Oyanagi 10.1186/s40645-023-00568-w
- Asbestos Hazard in Serpentinite Rocks: Influence of Mineralogical and Structural Characteristics on Fiber Potential Release L. Marzini et al. 10.3390/geosciences14080210
- Sr isotopes in metasomatized fault rocks constrain the age of juxtaposition of oceanic and continental lithosphere (Dun Mountain Ophiolite, New Zealand) M. Palmer et al. 10.1016/j.epsl.2023.118188
- Crystallographic preferred orientation of talc determined by an improved EBSD procedure for sheet silicates: Implications for anisotropy at the slab–mantle interface due to Si-metasomatism T. Nagaya et al. 10.2138/am-2020-7006
- Structural controls on the location, geometry and longevity of an intraplate volcanic system: the Tuatara Volcanic Field, Great South Basin, New Zealand T. Phillips & C. Magee 10.1144/jgs2020-050
- An updated catalogue of New Zealand’s mantle peridotite and serpentinite J. Scott 10.1080/00288306.2020.1776738
- From peridotite to listvenite – perspectives on the processes, mechanisms and settings of ultramafic mineral carbonation to quartz-magnesite rocks M. Menzel et al. 10.1016/j.earscirev.2024.104828
- Origin and evolution of nephrites, diopsidites and giant diopside crystals from the contact zones of the Pounamu Ultramafics, Westland, New Zealand A. Cooper 10.1080/00288306.2022.2050771
- An evolutionary model and classification scheme for nephrite jade based on veining, fabric development, and the role of dissolution–precipitation M. Tarling et al. 10.1038/s41598-022-11560-7
- Shear Zone Development in Serpentinized Mantle: Implications for the Strength of Oceanic Transform Faults S. Cox et al. 10.1029/2020JB020763
17 citations as recorded by crossref.
- Element and Sr–O isotope redistribution across a plate boundary-scale crustal serpentinite mélange shear zone, and implications for the slab-mantle interface J. Scott et al. 10.1016/j.epsl.2019.06.034
- Crystallographic orientation mapping of lizardite serpentinite by Raman spectroscopy M. Tarling et al. 10.5194/ejm-34-285-2022
- Evolution of a Normal Fault System Along Eastern Gondwana, New Zealand T. Sahoo et al. 10.1029/2020TC006181
- Heterogeneity in Microseismicity and Stress Near Rupture‐Limiting Section Boundaries Along the Late‐Interseismic Alpine Fault E. Warren‐Smith et al. 10.1029/2022JB025219
- Fluid overpressure from chemical reactions in serpentinite within the source region of deep episodic tremor M. Tarling et al. 10.1038/s41561-019-0470-z
- The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling T. Phillips et al. 10.5194/se-14-369-2023
- Rheology of Naturally Deformed Antigorite Serpentinite: Strain and Strain‐Rate Dependence at Mantle‐Wedge Conditions C. Tulley et al. 10.1029/2022GL098945
- Slip and stress in block-in-matrix shear zones: 1. microstructure and mineralogy of a serpentine-filled dilational jog S. Smith et al. 10.1016/j.jsg.2024.105220
- Geological fingerprints of deep slow earthquakes: A review of field constraints and directions for future research J. Platt et al. 10.1130/GES02722.1
- Si- versus Mg-metasomatism at the crust–mantle interface: insights from experiments, natural observations and geochemical modeling A. Okamoto & R. Oyanagi 10.1186/s40645-023-00568-w
- Asbestos Hazard in Serpentinite Rocks: Influence of Mineralogical and Structural Characteristics on Fiber Potential Release L. Marzini et al. 10.3390/geosciences14080210
- Sr isotopes in metasomatized fault rocks constrain the age of juxtaposition of oceanic and continental lithosphere (Dun Mountain Ophiolite, New Zealand) M. Palmer et al. 10.1016/j.epsl.2023.118188
- Crystallographic preferred orientation of talc determined by an improved EBSD procedure for sheet silicates: Implications for anisotropy at the slab–mantle interface due to Si-metasomatism T. Nagaya et al. 10.2138/am-2020-7006
- Structural controls on the location, geometry and longevity of an intraplate volcanic system: the Tuatara Volcanic Field, Great South Basin, New Zealand T. Phillips & C. Magee 10.1144/jgs2020-050
- An updated catalogue of New Zealand’s mantle peridotite and serpentinite J. Scott 10.1080/00288306.2020.1776738
- From peridotite to listvenite – perspectives on the processes, mechanisms and settings of ultramafic mineral carbonation to quartz-magnesite rocks M. Menzel et al. 10.1016/j.earscirev.2024.104828
- Origin and evolution of nephrites, diopsidites and giant diopside crystals from the contact zones of the Pounamu Ultramafics, Westland, New Zealand A. Cooper 10.1080/00288306.2022.2050771
2 citations as recorded by crossref.
- An evolutionary model and classification scheme for nephrite jade based on veining, fabric development, and the role of dissolution–precipitation M. Tarling et al. 10.1038/s41598-022-11560-7
- Shear Zone Development in Serpentinized Mantle: Implications for the Strength of Oceanic Transform Faults S. Cox et al. 10.1029/2020JB020763
Latest update: 21 Nov 2024
Short summary
Shear zones dominated by hydrated mantle rocks (serpentinites) occur in many tectonic settings around the world. To better understand the internal structure, composition and possible mechanical behaviour of these shear zones, we performed a detailed field, petrological and microanalytical study of the Livingstone Fault in New Zealand. We propose a conceptual model to account for the main physical and chemical processes that control deformation in large serpentinite shear zones.
Shear zones dominated by hydrated mantle rocks (serpentinites) occur in many tectonic settings...
