Item talk:Q312009
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Revised paleomagnetic pole for the Sonoma Volcanics, California", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70016116", "url": "https://pubs.usgs.gov/publication/70016116" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70016116 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1029/GL016i010p01081", "url": "https://doi.org/10.1029/GL016i010p01081" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "00948276" } ], "journal": { "@type": "Periodical", "name": "Geophysical Research Letters", "volumeNumber": "16", "issueNumber": "10" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Geophysical Research Letters" } ], "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", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-7496-2681", "url": "https://orcid.org/0000-0001-7496-2681" } } ] }
}