A structural metamorphic study of Broken Hill Block, NSW, Australia
The prograde pressure-temperature (P-T) path for the complexly polydeformed Proterozoic Broken Hill Block (Australia) has been reconstructed through detailed structural analysis in conjunction with calculation of compositionally specific P-T pseudosections of pelitic rock units within a hightemperature shear zone that formed early in the tectonic evolution of the terrane. Whilst the overall P-T path for the Broken Hill Block has been interpreted to be anticlockwise, the prograde portion of this...[Show more]
|Collections||ANU Research Publications|
|Source:||Journal of Metamorphic Geology|
|01_Forbes_A_structural_metamorphic_study_2005.pdf||3.18 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.