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• W1989366984 abstract "Synchronous deposition and deformation of the flysch deposits of eastern New York occurred during the westward overthrusting of the Taconic Allochthon in medial Ordovician time. An observed spatial west to east increase in the intensity of deformation is believed to represent the progressive development of structures through time. Folding initiated as upright kinks and buckles with fold axes north-south and approximately horizontal. Fold axes then rotated towards an east-west shear direction with fold tightness and asymmetry increasing and fold axial planes rotating to the west. Shear zones with a phacoidally cleaved fabric and small thrust faults strengthened the east over west structural asymmetry. After attaining intermediate dips (roughly 45°) the fold axial planes began to rotate back toward vertical and lose asymmetry. Bulk flattening and shear competed in the microstructural development of the flysch with slaty cleavage and phacoidal cleavage the corresponding end-products. Shear zones and thrust faults evolved into master faults, producing a large-scale imbricate structure in the flysch. Melange originated both as tectonically broken formations and as disrupted olistostromic deposits. The dominant mechanism for melunge formation appears to have been the disruption of interbedded graywacke and shale sequences under large strains. Imbrication of the original stratigraphic sequence has allowed the incorporation of older rocks, including shelf carbonate, into the melange as blocks and large slivers. The progressive sequence of structures observed within the flysch of eastern New York represents deformation within the leading edge of an accretionary prism developed over continental lithosphere." @default.
• W1989366984 created "2016-06-24" @default.
• W1989366984 creator A5000502182 @default.
• W1989366984 creator A5043695175 @default.
• W1989366984 date "1981-09-01" @default.
• W1989366984 modified "2023-10-13" @default.
• W1989366984 title "Structures of the Medial Ordovician Flysch of Eastern New York: Deformation of Synorogenic Deposits in an Overthrust Environment" @default.
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• W1989366984 doi "https://doi.org/10.1086/628622" @default.
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