Continental Thermal Blanketing Explains the Compositional Dichotomy of the Diffuse Basaltic Province...
Continental Thermal Blanketing Explains the Compositional Dichotomy of the Diffuse Basaltic Province Across Central‐Eastern Asia
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Washington: John Wiley & Sons, Inc
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Language
English
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Washington: John Wiley & Sons, Inc
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Contents
A diffuse magmatic province covering central‐eastern Asia continent displays a compositional transition at 120–100 Ma and probably reflects melting initiation in isotopically enriched lithospheric mantle, followed by melting of the asthenosphere. However, the cause for the transition across such a vast landmass remains poorly constrained. Here, ana...
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Continental Thermal Blanketing Explains the Compositional Dichotomy of the Diffuse Basaltic Province Across Central‐Eastern Asia
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TN_cdi_doaj_primary_oai_doaj_org_article_737b296c27044bfaaf56ffbbb7eef267
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_737b296c27044bfaaf56ffbbb7eef267
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ISSN
0094-8276
E-ISSN
1944-8007
DOI
10.1029/2023GL104951
