Zircon Lu-Hf isotopic compositions of the Paleoproterozoic meta-mafic and felsic rock assemblages in the Daqingshan complex: constraints on crustal evolution of the Khondalite Belt, north China Craton
Nowadays, the Khondalite Belt is considered to be a typical continent-continent collisional belt, formed by the collision of the Yinshan Block and the Ordos Block at 1.95–1.85 Ga. However, the pre-collisional tectonic setting and crustal evolutionary history of the Khondalite Belt are poorly constra...
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| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Frontiers Media S.A.
2025-06-01
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| Series: | Frontiers in Earth Science |
| Subjects: | |
| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2025.1632499/full |
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