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Lower oceanic crust formed by in situ melt crystallisation revealed by seismic layering
Oceanic crust forms at mid-ocean spreading centres through a combination of magmatic and tectonic processes, with the magmatic processes creating two distinct layers: the upper and the lower crust. While the upper crust is known to form from lava flows and basaltic dikes based on geophysical and dri...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7613063/ https://www.ncbi.nlm.nih.gov/pubmed/35855838 http://dx.doi.org/10.1038/s41561-022-00963-w |