Abstract
In the Proterozoic Mount Isa inlier, Queensland, Australia, structures belonging to an early brittle deformation event are overprinted and strongly disturbed by a phase of ductile east-west shortening. Many of these early structures have been attributed to thrusting, but data from the southern part of the inlier provide new evidence for extensional faulting. Analysis of the internal geometry of imbricates can provide a tool for the reconstruction of these strongly reworked Precambrian fault belts.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
