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At mid-ocean ridges, oceanic crust is emplaced in a narrow neovolcanic region on the seafloor, whereas basaltic melt that forms this oceanic crust is generated in a wide region beneath as suggested by a few geophysical surveys. The combined observati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::155a5bb9cea4c4c8bcbdbe0bf2661466
https://eartharxiv.org/uw7dn
https://eartharxiv.org/uw7dn
