| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4733570 | Journal of Structural Geology | 2011 | 23 Pages |
Abstract
⺠Diffuse partial melting in the lower crust does not obliterate earlier events. ⺠Pre-migmatic grain scale fabrics and foliations manifest fossil mineral equilibria. ⺠Mappable deformation histories drive sampling of metamorphic re-equilibration steps. ⺠Quality P-T-relative time of deformation paths (PTdt) are coherently derived. ⺠Rodinia break-up, subduction and exhumation signatures are inferred in Thor-Odin dome.
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Authors
M. Iole Spalla, Davide Zanoni, Paul F. Williams, Guido Gosso,