Abstract: P wave receiver functions reveal thinner mantle transition zone and low crustal velocity layer beneath Longqi hydrothermal vent at the ultra-slow spreading Southwest Indian Ridge (2016 AGU Fall Meeting)

P wave receiver functions reveal thinner mantle transition zone and low crustal velocity layer beneath Longqi hydrothermal vent at the ultra-slow spreading Southwest Indian Ridge

Hao Hu¹, Aiguo Ruan², Jiabiao Li³, Xiongwei Niu³, Xiaodong Wei⁴, Jie Zhang² and Aoxing Wang², (1)Zhejiang University, Department of Earth Science, Hangzhou, China, (2)Second Institute of Oceanography, State Oceanographic Administration of China, Hangzhou, China, (3)Second Institute of Oceanography, Ministry of Natural Resources, Key Laboratory of Submarine Geosciences, Hangzhou, China, (4)Second Institute of Oceanography, Ministry of Natural Resources, China, Hangzhou, China

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