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    New jurassic paleomagnetic data from Northern ssouth Aamerica: implications for the central atlantic opening
    Márcia ErnestoIgor Ivory Gil PaccaR. Siqueira
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    Tectonic implications of remagnetized upper Paleozoic strata of the northern Sierra Nevada
    Geology (1980)
    Judith L. HannahKenneth L. Verosub
    Research Article| November 01, 1980 Tectonic implications of remagnetized upper Paleozoic strata of the northern Sierra Nevada Judith L. Hannah; Judith L. Hannah 1Department of Geology, University of California, Davis, Davis, California 95616 Search for other works by this author on: GSW Google Scholar Kenneth L. Verosub Kenneth L. Verosub 1Department of Geology, University of California, Davis, Davis, California 95616 Search for other works by this author on: GSW Google Scholar Author and Article Information Judith L. Hannah 1Department of Geology, University of California, Davis, Davis, California 95616 Kenneth L. Verosub 1Department of Geology, University of California, Davis, Davis, California 95616 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1980) 8 (11): 520–524. https://doi.org/10.1130/0091-7613(1980)8<520:TIORUP>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Judith L. Hannah, Kenneth L. Verosub; Tectonic implications of remagnetized upper Paleozoic strata of the northern Sierra Nevada. Geology 1980;; 8 (11): 520–524. doi: https://doi.org/10.1130/0091-7613(1980)8<520:TIORUP>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A paleomagnetic study of a remagnetized Paleozoic terrane in the northern Sierra Nevada has provided new data on Cenozoic tectonics in the western United States. A combination of paleomagnetic and geologic evidence establishes that the remagnetization occurred during Late Jurassic time and that the rocks have experienced no major tectonic movement since. This conclusion establishes an eastern limit for the extent of large-scale tectonic rotations recently reported for Tertiary units on the western edge of the North American continent. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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    Paleomagnetic results from some Permian‐Triassic rocks from southwestern China
    Geophysical Research Letters (1984)
    Lung S. ChanChi-Young WangXue Yi Wu
    The Ailao Shan fault zone in West Yunnan represents a suture boundary between South China and Indosinian Cratons. Preliminary paleomagnetic results from three sites in Sichuan, Guichou, and Yunnan Provinces reveal a 14° northward migration of South China Craton between Late Permian and Middle Triassic. The two cratons were separated by about 20° latitudes during the Early Triassic. The tectonic setting of East Asia during the Triassic was probably analogous to the present Indonesian region.
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    A Paleomagnetic Study of Sediments from Site 397 Northwest African Continental Margin
    U.S. Government Printing Office eBooks (1979)
    N. Hamilton
    A magnetic polarity stratigraphy is established for the sediments of Site 397, which is located on the northwest African continental margin off Cape Bojador at the continental rise/slope juncture.The magnetic stratigraphy can be correlated with established geomagnetic polarity time-scales by some use of concurrent biostratigraphy control.The combination of magnetic stratigraphy with a good biostratigraphy allows for a more precise dating of important paleoenvironmental events in the development of this part of the northwest African continental margin in Neogene and Quaternary times.Sediment accumulation rates can be inferred from the detailed magnetic stratigraphy.Below the major hiatus encountered at this site, the Early Cretaceous sediments show predominantly normal magnetic polarity.Correlation to an established polarity time scale indicates probably an uppermost early Hauterivian age.
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