An Ediacaran orogeny in subglacial East Antarctica is uncovered by detrital garnet geochronology
Abstract Detrital minerals provide valuable insights into the tectonic history of continents. Uranium-lead dating of detrital zircon is widely used to characterize the magmatic history of continents but is generally insensitive to metamorphism accompanying the production and reworking of crust durin...
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| Päätekijät: | , , , , , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Nature Portfolio
2024-06-01
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| Sarja: | Communications Earth & Environment |
| Linkit: | https://doi.org/10.1038/s43247-024-01467-8 |
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