{
"USGS Publications Warehouse": {
"@context": "https://schema.org",
"@type": "Article",
"additionalType": "Journal Article",
"name": "Revised paleomagnetic pole for the Sonoma Volcanics, California",
"identifier": [
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"@type": "PropertyValue",
"propertyID": "USGS Publications Warehouse IndexID",
"value": "70016116",
"url": "https://pubs.usgs.gov/publication/70016116"
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"propertyID": "USGS Publications Warehouse Internal ID",
"value": 70016116
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"propertyID": "DOI",
"value": "10.1029/GL016i010p01081",
"url": "https://doi.org/10.1029/GL016i010p01081"
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"propertyID": "ISSN",
"value": "00948276"
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],
"journal": {
"@type": "Periodical",
"name": "Geophysical Research Letters",
"volumeNumber": "16",
"issueNumber": "10"
},
"inLanguage": "en",
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"@type": "CreativeWorkSeries",
"name": "Geophysical Research Letters"
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],
"datePublished": "1989",
"dateModified": "2024-02-13",
"abstract": "Paleomagnetic sampling of the Miocene and Pliocene Sonoma Volcanics, northern California, was undertaken to supplement an earlier collection. Data from 25 cooling units yield positive fold and reversal tests, and a paleomagnetic pole located at 80.2\u00b0N., 069.2\u00b0E., with \u03b195\u00a0= 6.8\u00b0. This paleopole is significantly displaced (9.6\u00b0 \u00b1 5.3\u00b0 of latitude) to the farside of the geographic pole. A highly elliptical distribution of the data in both direction and VGP space indicates that incomplete averaging of geomagnetic secular variation is a more likely explanation for this anomaly than is northward translation of the volcanic field.",
"description": "4 p.",
"publisher": {
"@type": "Organization",
"name": "American Geophysical Union"
},
"author": [
{
"@type": "Person",
"name": "Mankinen, E. A.",
"givenName": "E. A.",
"familyName": "Mankinen",
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"value": "0000-0001-7496-2681",
"url": "https://orcid.org/0000-0001-7496-2681"
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}