Research Article
Permeability Changes Resulting from Quartz Precipitation and Dissolution around Upper Crustal Intrusions
Figure 11
Fluid temperature at the center of an intrusion emplaced at 2 km depth, comparing systems without quartz precipitation and dissolution and a primary porosity of 0.1 with systems including quartz precipitation and dissolution and a primary porosity of 0.1, 0.05, or 0.025.