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Two deep-mantle sources for Paleocene doming and volcanism in the North Atlantic
The North Atlantic Igneous Province (NAIP) erupted in two major pulses that coincide with the continental breakup and the opening of the North Atlantic Ocean over a period from 62 to 54 Ma. The unknown mantle structure under the North Atlantic during the Paleocene represents a major missing link in...
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| Pubblicato in: | Proc Natl Acad Sci U S A |
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| Autori principali: | , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2019
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6612917/ https://ncbi.nlm.nih.gov/pubmed/31196961 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1816188116 |
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