Neoarchean (2.5–2.8 Ga) crustal growth of the North China Craton revealed by zircon Hf isotope: A synthesis
The crustal growth of the North China Craton (NCC) during the Neoarchean time (2.5–2.8 Ga) is a hotly controversial topic, with some proposing that the main crustal growth occurred in the late Neoarchean (2.5–2.6 Ga), in agreement with the time of the magmatism, whereas others suggest that the main...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Elsevier
2012-03-01
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| Series: | Geoscience Frontiers |
| Subjects: | |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S1674987111001101 |
