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    Palaeomagnetic and biostratigraphic dating of marine sediments from the Scotia Sea, Antarctica: First identification of the Laschamp excursion in the Southern Ocean
    Quaternary Geochronology (2011)
    Lewis CollinsMark W. HounslowClaire S. AllenDominic A. HodgsonJennifer PikeVassil Karloukovski
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    Geology and Paleoclimatology Research
    Geomagnetism and Paleomagnetism Studies
    Paleontology and Stratigraphy of Fossils
    Palaeomagnetic and biostratigraphic dating of marine sediments from the Scotia Sea, Antarctica: First identification of the Laschamp excursion in the Southern Ocean
    Quaternary Geochronology (2011)
    Lewis CollinsMark W. HounslowClaire S. AllenDominic A. HodgsonJennifer Pike
    Excursion
    Citations (21)
    Palaeomagnetism of Neoproterozoic glacial rocks of the Huabei Shield: the North China Block in Gondwana
    Journal of African Earth Sciences (1998)
    Apparent polar wander
    Polar wander
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    Late Quaternary geomagnetic stratigraphy recorded in Lake Erie sediments
    Earth and Planetary Science Letters (1976)
    K. M. CreerT. W. AndersonC F M Lewis
    Excursion
    Magnetostratigraphy
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    New paleomagnetic results for Ordovician and Silurian rocks of the Tarim Block, Northwest China and their paleogeographic implications
    Tectonophysics (2019)
    Baochun HuangJ. D. A. PiperLisha SunQian Zhao
    Continental Margin
    Red beds
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    Late Triassic initial closure of the Mongol-Okhotsk Ocean in the western segment: Constraints from sedimentological, detrital zircon ages and paleomagnetic evidence
    Gondwana Research (2023)
    Pan ZhaoZhenghua JiaBei XuYan XuTurbold Sukhbaatar
    Early Triassic
    Devonian
    Orogeny
    Late Devonian extinction
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    Early Paleozoic paleomagnetic poles from the western part of the North China Block and their implications
    Tectonophysics (1999)
    Baochun HuangZhenyu YangYo‐ichiro OtofujiRixiang Zhu
    Apparent polar wander
    Clockwise
    Polar wander
    Marine transgression
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    Paleomagnetism of the Ediacaran Avellaneda Formation (Argentina), Part II: Magnetic and chemical stratigraphy constraints on the onset of the Shuram carbon excursion
    Precambrian Research (2023)
    Jhon Willy Lopes AfonsoPablo R. FranceschinisAugusto E. RapaliniMaría Julia ArrouyLucía E. Gómez-Peral
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    Geomagnetic moment variation and paleomagnetic excursions since 400 kyr BP: a stacked record from sedimentary sequences of the Portuguese margin
    Earth and Planetary Science Letters (2004)
    Nicolas ThouvenyJulien CarcailletEva MorénoGuillaume LeducDavid Nérini
    Excursion
    Authigenic
    Magnetostratigraphy
    Geomagnetic secular variation
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    Paleomagnetism, Paleolatitudes, and Magnetic Overprinting on the North Slope, Alaska: ABSTRACT
    AAPG Bulletin (1985)
    D. B. Stone
    Several paleomagnetic studies have been made in Arctic Alaska, by industry, by the U.S. Geological Survey, and by the University of Alaska. In general, the results available to the public have been disappointing--most samples of pre-Cretaceous rocks give very steep magnetic inclinations with respect to present horizontal. This has been generally interpreted in terms of a Cretaceous overprinting event. A study of the paleomagnetism of Cretaceous rocks from the North Slope shows that although the Cretaceous field was steeply inclined, it was not as steep as conventional paleogeographic reconstructions would indicate, and not as steep as the bulk of the apparently remagnetized older rocks. This finding leaves open the possibility that the steeper directions recorded by the older rocks are the result of regional tilt, or the result of a paleogeography that allowed an earlier, steeper remagnetizing field. The shallower inclinations seen in the Cretaceous sediments of the Nanushuk Group (Albian-Cenomanian based on the fossil record with one K-Ar age of 100 Ma from an ash parting) give paleolatitudes of about 75°N. The predicted paleolatitude based on North American paleogeographic reconstructions is 80-85°N. Circumstantial evidence that the paleolatitude was shallower than 80-85°N comes from the enormous biogenic productivity needed to form the extensive coal deposits of the Nanushuk Group. Lower paleolatitudes also may be needed to explain the apparent existence of broad-leaved evergreens and the recently reported dinosaur tracks and skin imprints in the Nanushuk Group. End_of_Article - Last_Page 680------------
    Overprinting
    Citations (2)