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M. Beck, personal communication; E. Irving, personal communication. Irving has sampled in regions around Swartz Bay, Vancouver Island, and recognized a Tertiary overprint. All ammonites from the Haslam Formation in this region are recrystallized to calcite and black in color.
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personal communication. Irving has sampled in regions around Swartz Bay, Vancouver Island, and recognized a Tertiary overprint. All ammonites from the Haslam Formation in this region are recrystallized to calcite and black in color
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as a reason why previous paleomagnetic analyses of some Cordilleran rocks have yielded low inclinations
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Compaction shallowing is the phenomenon by which rotation, flattening, or compaction of sedimentary particles because of pressure from overlying strata causes a shifting of the magnetite particles within a bed, leading to spurious inclinations when ultimately sampled and analyzed. This effect was cited by R. F. Butler, W. R. Dickinson, and G. E. Gehrels [Tectonics 10, 561 (1991)] as a reason why previous paleomagnetic analyses of some Cordilleran rocks have yielded low inclinations.
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note
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We thank D. S. Cowan and R. T. Merril for reviewing the manuscript; J. Haggart, R. Enkin, and L. T. Silver for advice; L. Saul of the Los Angeles County Museum for guidance about California stratigraphy; and R. Lohman for assistance in running samples. Supported by NSF grants EAR-9372157 and EAR-9418283.
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