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: Tectonic and Geochronological Evolution of Orogens / reference | |||
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| Property / addresses subject: Climate Change and Paleoclimatology / rank | |||
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| Property / addresses subject: Climate Change and Paleoclimatology / reference | |||
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| Property / addresses subject: Magnetosome Formation in Prokaryotes / rank | |||
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| Property / addresses subject: Magnetosome Formation in Prokaryotes / reference | |||
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| Property / OpenAlex ID: W2041297839 / 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
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | 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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