Concordant paleolatitudes for Neoproterozoic ophiolitic rocks of the Trinity Complex, Klamath Mountains, California (Q143920): Difference between revisions

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Property / addresses subject: Tectonic and Geochronological Evolution of Orogens / rank
 
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Property / addresses subject: Magnetosome Formation in Prokaryotes / rank
 
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Latest revision as of 15:27, 12 September 2024

a Article (Journal Article) published by American Geophysical Union as part of series - Journal of Geophysical Research B: Solid Earth
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Concordant paleolatitudes for Neoproterozoic ophiolitic rocks of the Trinity Complex, Klamath Mountains, California
a Article (Journal Article) published by American Geophysical Union as part of series - Journal of Geophysical Research B: Solid Earth

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    OpenAlex ID
    W2041297839
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