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Formation and Evolution of the Continental Crust in North China Craton during Precambrian
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The North China Craton (NCC) preserves ancient rocks dating back to ca. 3.8 Ga, and has witnessed multiple magmatic–metamorphic events during the Archean–Proterozoic era. This critical period may have marked the transformation of the geodynamic regime on early Earth. As a result, the NCC serves as an ideal natural laboratory for deciphering the growth and evolution of continental crust, the onset of plate tectonics, and the architecture of the Archean geodynamic regime. To better understand the geological evolution of the NCC during the Precambrian, we collected 11 contributions for this Special Issue.
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Keywords
- AFC
- Alxa Block
- amphibolites
- crustal growth
- Dagushi Formation
- detrital zircon
- detrital zircon U-Pb ages
- early earth
- eastern Hebei Province
- extensional setting
- feature of source
- felsic metavolcanic rocks
- Geochemistry
- gneiss dome
- intra-continental rift
- Jiao-Liao-Ji Belt
- Khondalite Belt
- layered complex
- Lu-Hf isotopes
- monzogranitic dykes
- mylonite
- n/a
- NCC
- North China Craton
- North Liaohe Group
- Paleoproterozoic
- Paleoproterozoic Khondalite Belt
- Paleoproterozoic mafic rocks
- post-collisional granites
- provenance
- Qianlishan Complex
- sedimentary facies
- shear zone
- tectonic evolution
- tectonic setting
- the Alxa Block
- the Khondalite Belt
- TTG rocks
- U-Pb zircon dating
- UHT granulite/gneiss
- zircon U-Pb age
- zircon U-Pb chronology
- zircon U–Pb dating
Links
DOI: 10.3390/books978-3-7258-1949-2Editions