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Birth of an oceanic spreading center at a magma-poor rift system
Oceanic crust is continuously created at mid-oceanic ridges and seafloor spreading represents one of the main processes of plate tectonics. However, if oceanic crust architecture, composition and formation at present-day oceanic ridges are largely described, the processes governing the birth of a sp...
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| Pubblicato in: | Sci Rep |
|---|---|
| Autori principali: | , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2017
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5678130/ https://ncbi.nlm.nih.gov/pubmed/29118393 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-15522-2 |
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