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Autor:
Qing Xiong, Hongun Dai, Zheng Jianping, William Griffin, Hong-Da Zheng, Li Wang, Suzanne O'Reilly
Adiabatic decompressional melting of asthenosphere under spreading centers has been accepted to produce vertical compositional variations of oceanic lithospheric mantle. However, theoretical estimates of the compositional gradients are much smaller t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cb5a47ae89f7a1598da1e4f87f6a341
https://doi.org/10.21203/rs.3.rs-1394420/v1
https://doi.org/10.21203/rs.3.rs-1394420/v1