Formation and crust-mantle geodynamic processes of the Neoarchean K-Rich granitoid belt in the Southern Range of Eastern Hebei-Western Liaoning Provinces, North China Craton [electronic resource] : Neoarchean K-Rich Granitoid Belt in the Northern North China Craton / Jinghao Fu.
Meso- to Neoarchean is a critical transitional period for the formation and evolution of continental crust and the corresponding geodynamic mechanisms, during which the average composition of continental crust gradually shifted from Na-enriched to K-enriched. However, the ultimate source of K and it...
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| Format: | Electronic eBook |
| Language: | English |
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Singapore :
Springer,
2022.
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| Series: | Springer theses.
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Internet
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| Call Number: |
QE653.3
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| QE653.3 | Available |