| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4713982 | Journal of Volcanology and Geothermal Research | 2007 | 12 Pages |
Abstract
An interesting, still unexplained phenomenon has been detected during transient phases when both pressure and temperature gradients were applied to the samples. The phenomenon consists in an enhancement of volume flux due to heat flux in the transient phase. The extra volume-flux disappears once the steady temperature gradient is reached.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
F. Peluso, I. Arienzo,