Subduction-zone crust-mantle interaction is a common mechanism for the origin of oceanic arc and island basalts

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ADS bibcode
2014AGUFM.S51B4457Z
year
2014
Listed Authors
Zheng, Y. F.
Zhao, Z. F.
Listed Institutions
University of Science and Technology of China, Hefei, China
University of Science and Technology of China, Hefei, China

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