Formation of the 15 Å phase as the most expanded hydrated mineral in cold subduction zone
Formation of the 15 Å phase as the most expanded hydrated mineral in cold subduction zone
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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Talc, as an important class of clay minerals constituting subducting oceanic crust, has long been known to undergo interlayer expansion by ~6% to contain net ~13 wt.% water into the ‘so-called’ 10 Å phase. Although subduction fluid is mildly alkaline and includes various salts and other dissolved species, its effect on the stability of subducting m...
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Formation of the 15 Å phase as the most expanded hydrated mineral in cold subduction zone
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TN_cdi_doaj_primary_oai_doaj_org_article_a7ffd1911dcf4746b6a20c3941fa0270
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_a7ffd1911dcf4746b6a20c3941fa0270
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2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-025-56672-6
