An oceanic subduction origin for Archaean granitoids revealed by silicon isotopes
An oceanic subduction origin for Archaean granitoids revealed by silicon isotopes
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London: Nature Publishing Group UK
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English
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Publisher
London: Nature Publishing Group UK
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Modern oceanic crust is constantly produced at oceanic ridges and recycled back into the mantle at subduction zones via plate tectonics. An outstanding question in geology is whether the Earth started in a non-plate tectonic regime, and if it did, when the transition to the modern regime occurred. This is a complicated question to address because A...
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An oceanic subduction origin for Archaean granitoids revealed by silicon isotopes
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TN_cdi_hal_primary_oai_HAL_hal_02278676v1
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_02278676v1
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ISSN
1752-0894
E-ISSN
1752-0908
DOI
10.1038/s41561-019-0407-6
