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...
| Egile Nagusiak: | , , , , , |
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| Formatua: | Artikulua |
| Hizkuntza: | English |
| Argitaratua: |
Nature Portfolio
2024-06-01
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| Saila: | Communications Earth & Environment |
| Sarrera elektronikoa: | https://doi.org/10.1038/s43247-024-01467-8 |