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- W2084133311 abstract "Abstract A compound tectonic fabric is associated with folded and faulted calcareous mudrock in the foreland fold-and thrust-belt of the Appalachian orogen. Two approximately coplanar spaced cleavages evolved during one episode of folding. An earlier close-spaced (40 μ spacing) domainal microfabric is overprinted by, and transitional with a wider spaced (2–3 cm spacing), spaced-disjunctive cleavage. Development of the spaced cleavage from the domainal microfabric is considered due to a change in dominant deformation-mode from controlled grain-boundary sliding to pressure-solution. Factors which determine whether single or compound cleavage fabrics develop in singly folded rocks may relate to the timing of cleavage-forming deformation increments relative to metamorphic dehydration-reactions. At low metamorphic grade (anchimetamorphism to low greenschist facies) it is proposed that grain-alignment cleavage will develop when reactions are concomitant with deformation, whereas a spaced cleavage will develop when reactions are inhibited or have gone to completion. Compound tectonic fabrics result when reactions either undergo completion or are initiated during the period of cleavage formation. There are three distinct geometrical associations of compound fabrics and folds. These associations are determined by the relative timing of formation of the various cleavages with respect to the folding." @default.
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- W2084133311 date "1981-10-01" @default.
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- W2084133311 title "Compound tectonic fabrics in singly folded rocks from southwest Virginia U.S.A." @default.
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- W2084133311 doi "https://doi.org/10.1016/0040-1951(81)90015-9" @default.
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