Precambrian evolution of the Quanji Block, northeastern margin of Tibet: Insights from zircon U–Pb and Lu–Hf isotope compositions

Author:

Chen Nengsong,Gong Songlin,Sun Min,Li Xiaoyan,Xia Xiaoping,Wang Qinyan,Wu Fuyuan,Xu Ping

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference71 articles.

1. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons;Amelin;Nature,1999

2. Igneous zircon: trace element composition as an indicator of source rock type;Belousova;Contributions to Mineralogy and Petrology,2002

3. Zircon crystal morphology, trace element signatures and Hf isotope composition as a tool for petrogenetic modeling: examples from eastern Australian granitoids;Belousova;Journal of Petrology,2006

4. The Lu–Hf geochemistry of chondrites and the evolution of the mantle–crust system;Blichert-Toft;Earth and Planetary Science Letters,1997

5. LA-ICP-MS U–Pb zircon dating for Felsic Granulite, Huangtuling area, North Dabieshan: constraints on timing of its protolith and granulite-facies metamorphism, and thermal events in its provenance;Chen;Journal of China University of Geosciences,2005

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