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- W2087675963 abstract "Four phases of deformation are recorded by minor structures in the New Harbour Group (NHG) of southern Holy Island. The regional schistosity in these rocks is a differentiated crenulation cleavage of D2 age. An earlier preferred orientation (S1) is commonly preserved as crenulations within the Q-domain microlithons of the S2 schistosity and is demonstrably non-parallel to bedding. F3 folds are widely developed in S2 and, to a lesser extent, in bedding. S3 crenulation cleavage is sporadically developed but can be intense locally. A major antiformal fold exists in the NHG near Rhoscolyn. This fold is of D3 age since it clearly deforms S2 schistosity and is consistent with the vergence of F3 minor structures. All planar structures are deformed by folds of D4 age. © 1997 John Wiley & Sons, Ltd." @default.
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- W2087675963 date "1997-06-01" @default.
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- W2087675963 title "On the deformation sequence in the New Harbour Group of Holy Island, Anglesey, North Wales" @default.
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- W2087675963 doi "https://doi.org/10.1002/(sici)1099-1034(199706)32:2<119::aid-gj733>3.0.co;2-j" @default.
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