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• W2084073817 abstract "Results of a study of calcite-twin analysis and anisotropy of anhysteretic remanent magnetization (AARM) for the Onondaga Limestone in the Hudson Valley Fold and Thrust belt (HVB), raise questions about the deformation history of this area and the nature of AARM. Two bedding parallel shortening directions are inferred from calcite twinning: one normal to HVB fold axes, NW-SE to ENE-WSW, and the other at high angles to this direction, NNE-SSW to N-S. Two hypotheses are put forward to explain the inconsistent shortening direction: (1) even during the initial stages of folding and thrusting in the HVB, deformation was three-dimensional in character; (2) the HVB developed synchronous with Main phase Alleghanian deformation. AARM results are consistent with the magnetic anisotropy being in part caused by the deformation associated with folding and thrusting. This is a surprising result because the magnetization is presumably of diagenetic origin, and it was acquired after folding." @default.
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• W2084073817 date "1993-01-01" @default.
• W2084073817 modified "2023-10-16" @default.
• W2084073817 title "Deformation and magnetization of the Hudson Valley, eastern New York: Results of a study of calcite twinning and anisotropy of magnetic remanence in the Onondaga Limestone" @default.
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• W2084073817 doi "https://doi.org/10.1016/0040-1951(93)90013-a" @default.
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