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- W2183320007 abstract "We measured the Paleomagnetism of 53 limestone samples recovered from Hole 865A, atop Allison Guyot in the Mid-Pacific Mountains, to place constraints on the paleolatitude of the edifice near the time of its formation. Most samples were recovered from the bottom of the hole, in a section of Albian (probable early Albian) clayey limestone deposited in a marshy, nearshore environment and intruded by several basaltic sills while soft. Natural remanent magnetization (NRM) intensities displayed a large range, varying byjnore than five orders of magnitude and generally decreasing upsection. The NRM intensities probably reflect the concentration of volcanic grains, eroded from a nearby volcanic high and deposited in the sediments. Saturation of isothermal remanent magnetizations in low applied fields and moderate mean destructive field values are consistent with titanomagnetite as the dominant magnetic grain type in these limestones. Nearly all samples showed stable behavior during alternating field (AF) demagnetization and gave apparently reliable characteristic remanence directions. A mean inclination of-26.8° (95% confidence limits: -24.4°, -28.7°; k = 75; N = 51) implies a paleolatitude of 14.2° ± 1.3°S. This value is statistically indistinguishable from that inferred from the mid-Cretaceous Pacific apparent polar wander path (APWP), suggesting that the paleolatitude is reliable." @default.
- W2183320007 created "2016-06-24" @default.
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- W2183320007 date "1995-05-01" @default.
- W2183320007 modified "2023-09-24" @default.
- W2183320007 title "Paleolatitude Inferred from Cretaceous Sediments, Hole 865A, Allison Guyot, Mid-Pacific Mountains" @default.
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- W2183320007 doi "https://doi.org/10.2973/odp.proc.sr.143.250.1995" @default.
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