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Volumn 277, Issue 5332, 1997, Pages 1642-1645

Measurements of the Cretaceous paleolatitude of Vancouver island: Consistent with the Baja-British Columbia hypothesis

Author keywords

[No Author keywords available]

Indexed keywords

BAJA-BRITISH COLUMBIA; BIOSTRATIGRAPHY; CRETACEOUS; PALAEOMAGNETISM; TECTONIC RECONSTRUCTION;

EID: 0030802714     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.277.5332.1642     Document Type: Article
Times cited : (76)

References (33)
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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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    • 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
    • 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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