Titanium isotopes constrain a magmatic transition at the Hadean-Archean boundary in the Acasta Gneiss Complex

Plate subduction greatly influences the physical and chemical characteristics of Earth’s surface and deep interior, yet the timing of its initiation is debated because of the paucity of exposed rocks from Earth’s early history. We show that the titanium isotopic composition of orthogneisses from the...

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Detalles Bibliográficos
Autores principales: Aarons, Sarah M., Reimink, Jesse R., Greber, Nicolas D., Heard, Andy W., Zhang, Zhe, Dauphas, Nicolas
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2020
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7725461/
https://www.ncbi.nlm.nih.gov/pubmed/33298445
http://dx.doi.org/10.1126/sciadv.abc9959

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7725461/
https://www.ncbi.nlm.nih.gov/pubmed/33298445
http://dx.doi.org/10.1126/sciadv.abc9959

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