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Water-rock interaction experiment with samples derived from the granites shows wide range of geochemical variation.
Figure 2 Geochemical variation of liquids of the Izu-Oshima volcano.
Figure 5 Piper ([1944]) trilinear diagram, showing the geochemical variation of different water types from study area.
We investigated the origins of geochemical variation in volcanic rocks having multiple phase saturated liquid compositions from the Izu-Oshima volcano in the northern Izu arc.
The geochemical variation patterns of Mo in plants are similar to those in soils, which suggest a corresponding Mo anomaly and enhanced contrast near the Mo orebodies.
The dominant hydrochemical facies of groundwater in the study area is Ca Mg SO4 Cl, Ca HCO3, and Na Cl types indicating the geochemical variation along the groundwater flow path.
Similar(49)
Few geochemical variations of the Mudeungsan Tuff indicate that tuff originated from a single magma chamber.
Geochemical variations in fluids can also provide support in decline rate studies of wells.
The geochemical variations in the liquids fall between two endmember trends, namely higher- and lower-Al/Si trends.
The geochemical variations in the ionic concentrations in the groundwater can easily be understood when they are plotted along an X Y coordinate (Guler et al. 2002).
The geochemical variations in the ionic concentrations in the surface water can easily be understood when they are plotted along an X Y coordinate.
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