1
زمینشناسی و معدن::
مایع منفذی
Additionally, the pore fluid pressure increases due to additional water contained in opal that is released from
Methane and other volatile hydrocarbons are generated from decomposing organic material and add to the increase in pore fluid pressure (Kopf, 2003).
The water, which originally occurred as pore fluids and in hydrated minerals, is forced out of the highly strained subduction zone upward through the accretionary prism.
Recall from above that pore fluids originate both from de- watering of hydrous minerals and from expulsion of water from sediments.
Pore fluids in the high-stress zone along the plate boundary decollement actually increase mobility and slippage in this zone by acting as a lubricant.
واژگان شبکه مترجمین ایران