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- W2093349027 abstract "Magnetization measurements were made on a hundred-twelve independently oriented cores drilled at twenty-two sites distributed among six basic intrusive plugs forming part of the Monteregian Hills group in southeast Quebec. On the basis of adopted magnetization homogeneity criteria, less than 80% of the sampled cores were accepted as reliable carriers of paleomagnetic information, after af cleaning in a peak demagnetizing field of 250 oe. An analysis of the data obtained from these cores representative of sixteen sites yielded a mean direction of magnetization whose declination and inclination are, respectively, 157.4° and −59.9°. The circle of confidence about the resultant of the sixteen ‘weighted’ site means has a radius α′.95 equal to 3.3°. No reliable evidence of mixed polarity in the paleomagnetic directions within any one of the six intrusives studied was found, although additional evidence was obtained to postulate at least one earth's field reversal during their formation. Combining the above mentioned data with seventy-five previously reported core mean directions representative of sixteen sites on four other members of the Monteregian Hills group yielded a paleomagnetic pole position at 170.5°W, 71.3°N. The low angular standard deviation of the thirty-two ‘weighted’ site means summarizing these data (7.8°) suggests that the non-dipole component of the earth's magnetic field was less important in Cretaceous time than it was over the last 10 m.y." @default.
- W2093349027 created "2016-06-24" @default.
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- W2093349027 date "1969-05-15" @default.
- W2093349027 modified "2023-09-27" @default.
- W2093349027 title "Paleomagnetism of the Monteregian Hills: Further new results" @default.
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- W2093349027 doi "https://doi.org/10.1029/jb074i010p02570" @default.
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