as the ratio of the mass flux of melt added to the oceanic crust to the mass flux of mantle entering the melting region; Forsyth (1993) has defined mean F as the average degree of melting of all pooled melt increments, with degree calculated at the last point of chemical equilibration. ...
We show that the thermal state (thermotectonic age) of the lithosphere is only one of at least three equally important properties that determine apparent values of Te. These other properties are the state of the crust-mantle interface (decoupling of crust and mantle), the thickness and ...
The thickness of the aquifer and the percentage of available sand increase from the north to the south of the region [41]. There is a substantial relationship between the amount of and the temporal variation in water vapor in the troposphere, as mentioned in the introduction. As a result, ...