Evidence for dominant grain-boundary sliding deformation in greenschist- and amphibolite-grade polymineralic ultramylonites from the Redbank Deformed Zone, Central Australia
- 1 December 1997
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 19 (12) , 1495-1520
- https://doi.org/10.1016/s0191-8141(97)00076-x
Abstract
No abstract availableKeywords
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