Nd-O-Hf isotopic decoupling in S-type granites: Implications for ridge subduction

Author:

Zhang Chen,Liu Dongdong,Zeng Jianhui,Jiang Shu,Luo Qun,Kong Xiangye,Yang Wei,Liu Luofu

Funder

National Natural Science Foundation of China

National Key R&D Program of China

National Science and Technology

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference89 articles.

1. Do S-type granites commonly sample infracrustal sources? New results from an integrated O, U–Pb and Hf isotope study of zircon;Appleby;Contributions to Mineralogy and Petrology,2010

2. A review of the relationships between granitoid types, their origins and their geodynamic environments;Barbarin;Lithos,1999

3. Regional Geology of Xinjiang Uygur Autonomous Region. People's Republic of China, Ministry of Geology and Mineral Resources;BGMRX (Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region),1993

4. Slab breakoff: a model for syncollisional magmatism and tectonics in the alps;Blanckenburg;Tectonics,1995

5. Zircon saturation re-revisited;Boehnke;Chemical Geology,2013

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