Formation and Evolution of the Continental Crust in North China Craton during Precambrian

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 a...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Egile korporatiboa: Liu, Jin, Qian, Jiahui, Liu, Xiaoguang
Formatua: Livro
Hizkuntza:Inglês
Argitaratua: MDPI - Multidisciplinary Digital Publishing Institute 2024
Gaiak:
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBG Geology, geomorphology and the lithosphere
NCC
Paleoproterozoic Khondalite Belt
UHT granulite/gneiss
layered complex
AFC
tectonic evolution
Alxa Block
North China Craton
TTG rocks
detrital zircon U-Pb ages
North Liaohe Group
provenance
Jiao-Liao-Ji Belt
monzogranitic dykes
U-Pb zircon dating
Lu-Hf isotopes
post-collisional granites
Dagushi Formation
sedimentary facies
detrital zircon
geochemistry
felsic metavolcanic rocks
intra-continental rift
early earth
eastern Hebei Province
crustal growth
gneiss dome
zircon U–Pb dating
Paleoproterozoic
Qianlishan Complex
Khondalite Belt
amphibolites
the Alxa Block
the Khondalite Belt
zircon U-Pb age
extensional setting
shear zone
mylonite
Paleoproterozoic mafic rocks
zircon U-Pb chronology
feature of source
tectonic setting
n/a
Sarrera elektronikoa:https://directory.doabooks.org/handle/20.500.12854/143745
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