U-Pb and Hf isotope analyses of zircons from felsic granulite xenoliths in Mesozoic volcanics reveal Early Archean (≥3.6 Ga) lower crust beneath the younger (<2.85 Ga) southern margin of the North China craton, and suggest that the eastern part of the craton formed a coherent block by 3.6 Ga. Hf model ages indicate extraction of protoliths from the mantle ca. 4 Ga or earlier, followed by remelting at 3.6–3.7 Ga. Hf isotope data require both recrystallization of magmatic zircons, and growth of new zircon, up to ca. 1.9 Ga. One sample records 2.1–1.9 Ga remelting of a 2.5 Ga protolith. If large parts of the exposed upper continental crust elsewhere also are underlain by older lower crust, estimates of crustal growth rates through time will re...
The eastern part of the North China Craton contains large volumes of Late Archean hornblenditic, ton...
The genetic links among rift magmatism, crustal growth and water–rock interaction are an important i...
Evidence for the earliest known terrestrial crust comes predominantly from Jack Hills in Western Aus...
Deep-seated xenoliths in volcanic rocks offer direct glimpses into the nature and evolution of the l...
It is generally recognized that the North China Craton (NCC) resulted from the amalgamation of sever...
Recent tectonic analysis suggests that the North China Craton consists of two Archean continental bl...
Knowledge of the lower crust beneath the southeastern parts of North China Craton (NCC) is still spa...
The age distribution of the crust is a fundamental parameter in modeling continental evolution and t...
The late Mesozoic granitoids widely distributed in the northwestern Jiaodong Terrane are important m...
The North China craton (NCC) was stabilized in Palco-Proterozoic times, and the eastern part of it w...
How has the Earth's continental lithosphere evolved? Most of our knowledge is derived from surface e...
How has the Earth's continental crust evolved? Most of our knowledge comes from surface exposures, b...
The collision between the North and South China cratons in Middle Triassic time (240-225 Ma) created...
Zircon xenocrysts from the Early Paleozoic Mengyin and Fuxian diamondiferous kimberlites, on opposit...
Zircon U-Pb-Hf-O data for lower-crustal xenoliths from Phanerozoic igneous rocks in the North China ...
The eastern part of the North China Craton contains large volumes of Late Archean hornblenditic, ton...
The genetic links among rift magmatism, crustal growth and water–rock interaction are an important i...
Evidence for the earliest known terrestrial crust comes predominantly from Jack Hills in Western Aus...
Deep-seated xenoliths in volcanic rocks offer direct glimpses into the nature and evolution of the l...
It is generally recognized that the North China Craton (NCC) resulted from the amalgamation of sever...
Recent tectonic analysis suggests that the North China Craton consists of two Archean continental bl...
Knowledge of the lower crust beneath the southeastern parts of North China Craton (NCC) is still spa...
The age distribution of the crust is a fundamental parameter in modeling continental evolution and t...
The late Mesozoic granitoids widely distributed in the northwestern Jiaodong Terrane are important m...
The North China craton (NCC) was stabilized in Palco-Proterozoic times, and the eastern part of it w...
How has the Earth's continental lithosphere evolved? Most of our knowledge is derived from surface e...
How has the Earth's continental crust evolved? Most of our knowledge comes from surface exposures, b...
The collision between the North and South China cratons in Middle Triassic time (240-225 Ma) created...
Zircon xenocrysts from the Early Paleozoic Mengyin and Fuxian diamondiferous kimberlites, on opposit...
Zircon U-Pb-Hf-O data for lower-crustal xenoliths from Phanerozoic igneous rocks in the North China ...
The eastern part of the North China Craton contains large volumes of Late Archean hornblenditic, ton...
The genetic links among rift magmatism, crustal growth and water–rock interaction are an important i...
Evidence for the earliest known terrestrial crust comes predominantly from Jack Hills in Western Aus...