Intracontinental Orogeny Enhanced by Far‐Field Extension and Local Weak Crust-Reference-Cited by-同舟云学术

Intracontinental Orogeny Enhanced by Far‐Field Extension and Local Weak Crust

Published:2018-12 Issue:12 Volume:37 Page:4421-4443
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Silva David¹^ORCID,Piazolo Sandra¹²^ORCID,Daczko Nathan R.¹^ORCID,Houseman Gregory²^ORCID,Raimondo Tom³⁴^ORCID,Evans Lynn⁵^ORCID

Affiliation:

1. ARC Centre of Excellence for Core to Crust Fluid Systems and GEMOC, Department of Earth and Planetary Sciences Macquarie University Sydney New South Wales Australia

2. School of Earth and Environment, Institute of Geophysics and Tectonics University of Leeds Leeds UK

3. School of Natural and Built Environments University of South Australia Adelaide South Australia Australia

4. Future Industries Institute University of South Australia Adelaide South Australia Australia

5. School of Earth, Atmosphere and Environmental Sciences Monash University Clayton Victoria Australia

Funder

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018TC005106

Reference94 articles.

1. The architecture, kinematics, and lithospheric processes of a compressional intraplate orogen occurring under Gondwana assembly: The Petermann orogeny, central Australia

2. Local stress fields and intraplate deformation of Iberia: variations in spatial and temporal interplay of regional stress sources

3. Exhumation of the lower crust during crustal shortening: an Alice Springs (380 Ma) age for a prograde amphibolite facies shear zone in the Strangways Metamorphic Complex (central Australia)

4. Deformation Fields Around A Fault Embedded In A Non-Linear Ductile Medium

5. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation

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