Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting
Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting
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Washington: John Wiley & Sons, Inc
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English
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Publisher
Washington: John Wiley & Sons, Inc
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Contents
Upper mantle anisotropy has been mapped beneath continents at high spatial resolution. Beneath the oceans, however, shear wave splitting constraints on upper mantle anisotropy are sparse, due to the paucity of seismic receivers. A technique that does not require the availability of seismic stations close to the region under study is differential PS...
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Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting
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TN_cdi_doaj_primary_oai_doaj_org_article_6695796b3c7f4f9689e3dee156f78058
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_6695796b3c7f4f9689e3dee156f78058
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ISSN
0094-8276
E-ISSN
1944-8007
DOI
10.1029/2023GL104402