| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4733594 | Journal of Structural Geology | 2011 | 12 Pages |
Abstract
⺠Zones of porphyroblastic rock preserve the effects of the numerous regional deformation events. ⺠FIAs are a product of folding events and their trends are controlled by folds with steep axial planes. ⺠FIA trends directly reflect folds that formed with steeply dipping axial planes. ⺠Regional fold trends have peaks coincident or within 10° of a succession of FIA peaks. ⺠FIAs provide the regional successions of folding preserving the orientations in which they formed.
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Geology
Authors
T.H. Bell, I.V. Sanislav,