Structure of the mantle transition zone beneath the North China Craton

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Structure of the mantle transition zone beneath the North China Craton

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作者：Shaokun Si^a ; Yanpeng Zheng^b ; Baohua Liu^a ; Xiaobo Tian^c ; ^d ; ^{txb@mail.iggcas.ac.cn" class="auth_mail" title="E-mail the corresponding author}
关键词：North China Craton ; Pacific plate subduction ; Receiver function ; Discontinuous thickening ; Mantle transition zone
刊名：Journal of Asian Earth Sciences
出版年：2016
出版时间：February 2016
年：2016
卷：116
期：Complete
页码：69-80
全文大小：4645 K

文摘

•: Discontinuous thickening of the MTZ beneath the NCC was imaged by seismic data.
•: A double 660 km discontinuity structure exists beneath the southeastern ENCC.
•: Pacific plate subduction and trench retreat result in stagnant slab in the MTZ.
•: Discontinuous thickening may be related to the subduction rate of the slab.

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