2018
DOI: 10.1186/s40623-018-0869-6
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Crustal dynamics: unified understanding of geodynamic processes at different time and length scales

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Cited by 4 publications
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“…The volatile gas content of mafic magma is relatively high, and the magma temperature can reach >1,100 °C (Iio et al, 2018). During overflow along the surface after magma eruption, gas escapes and forms many vesicles under the dual effects of temperature and pressure (He et al, 2019).…”
Section: Formation Mechanisms Of the Reservoirsmentioning
confidence: 99%
“…The volatile gas content of mafic magma is relatively high, and the magma temperature can reach >1,100 °C (Iio et al, 2018). During overflow along the surface after magma eruption, gas escapes and forms many vesicles under the dual effects of temperature and pressure (He et al, 2019).…”
Section: Formation Mechanisms Of the Reservoirsmentioning
confidence: 99%