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When crust comes of age: on the chemical evolution of Archaean, felsic continental crust by crustal drip tectonics
The secular evolution of the Earth's crust is marked by a profound change in average crustal chemistry between 3.2 and 2.5 Ga. A key marker for this change is the transition from Archaean sodic granitoid intrusions of the tonalite–trondhjemite–granodiorite (TTG) series to potassic (K) granitic...
Uloženo v:
| Vydáno v: | Philos Trans A Math Phys Eng Sci |
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| Hlavní autoři: | , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
The Royal Society Publishing
2018
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6189554/ https://ncbi.nlm.nih.gov/pubmed/30275165 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2018.0103 |
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