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A finite strain study of the Ordovician volcanic rocks of Snowdonia, North Wales, and its implications for a regional strain model
Author(s) -
Wilkinson Ian
Publication year - 1987
Publication title -
geological journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.721
H-Index - 54
eISSN - 1099-1034
pISSN - 0072-1050
DOI - 10.1002/gj.3350220510
Subject(s) - geology , strain (injury) , deformation (meteorology) , volcanic rock , finite strain theory , ordovician , volcano , shear (geology) , petrology , paleontology , finite element method , engineering , medicine , oceanography , structural engineering
A regional strain study of Snowdonia, North Wales, has used clast orientation data from Caradoc volcanic rocks. The data, analysed using the Rf /Φ technique, have revealed that while the local strain pattern is very heterogeneous in intensity and style, it can be processed to define a regional ‘average’ strain. This regional strain closely approximates to plane‐strain in both rigid and ductile markers. This, when considered with the style of folds, leads to the tentative suggestion that the deformation mechanism in Snowdonia is one of gently inclined and ductile simple shear from the northwest.