Hydrogeochemical simulation is an effective method to study water-rock interaction.In this paper, PHREEQM was used for the simulation of water-rock interaction
There exist intermediate to intermediate-acid shoshonitic rocks dated at 26.3 - 36.7Ma in the Early Tertiary extensional basins along the NE flank of the Dali-J
The West Kunlun orogenic belt is located at the conjunction of the paleo-Asian tectonic system and the Tethys tectonic system. Petrological and mineralogical st