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Observations of the time lag between the last deglaciation and a surge in volcanic activity in Iceland constrain the average melt ascent velocity to be $\geq50$ $\mathrm{m/yr}$. Although existing theoretical work has explained why the surge in erupti
Externí odkaz:
http://arxiv.org/abs/1902.00697
Autor:
Eksinchol, Isarapong
Volcanic eruption rates in Iceland during the last deglaciation increased 5--30 fold from the steady-state rates. This has been understood by the unloading of ice, which increases the decompression rates in the mantle, causing enhanced mantle melting
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02fe5c3f369bcd9093b2057084edb592