These fluids are similar in these characteristics to many of the Ba-rich, saline coalfield brines (Fig. ... Ca:Mg 6a20 times seawater, both indicating extensive fluid-rock interaction, including interaction with Li-rich basement rocks. ... This can be quantified through the Peclet number (Pe), which is a measure of the relative importance of fluid flow relative to thermal conduction in moving heat. ... We use these basic ideas to test the three models of hydrothermal ore genesis identified above.
|Title||:||Proceedings of the Yorkshire Geological Society|
|Author||:||Yorkshire Geological Society|