Mineral Resources Potential - Geothermal Resources
Mineral Resources Potential - Geothermal Resources
Mineral Resources Potential - Geothermal Resources
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Metallic <strong>Mineral</strong>s 39<br />
to 40O0c). The fluids use the fault/fracture zones as permeable<br />
channels along which to tow from their region of origin untii they<br />
reach a point where in any of a number of factors -chemical<br />
reactions with country rock andlor changes. in the temperature<br />
andlor pressure -causes the fluids to precipitate. The gold<br />
precipitates out of solution along with the quartz vein material.<br />
These regional fault systems develop during the waning stages of<br />
continental collision and hence can form at significantly later<br />
periods than the host rocks; as such, they are termed "epigenetic."<br />
The actual host rocks of the orogenic mesotl~ern~al lode<br />
deposits are affected by these fnultlfracture origins and can range<br />
fmn mylonites to fault gouge. Mylonites indicate deformation<br />
under confining pressures sufficiently high that the rock<br />
recrystallizes to a fine grain size. This is plastic or ductile<br />
behavior, and indicates that the vein formed deep in the earth's<br />
am@, Alternatively, if the faultlfrachlre cuts a rock at a level cIose<br />
, to the earth's surface, then it does not have the same confining<br />
pressure and hence will break into fault gouge.<br />
Typical orogenic mesothermal lode gold deposits consist of<br />
quark veins with gold, pyrite andlor arsenopyrite, The gold is<br />
usually pure gold and can be present in textures ranging from<br />
solitary grains to grains intimately ii~tergrown with sulphide<br />
minerals. In some deposits, gold is present as "invisible"<br />
intergrowths with suIphj& minerals such as arsenopycite (that is,<br />
the gold is in the crystal lattice of the sulphide mineral). In other<br />
deposits, the gold is not pure but electnun -a mineral made up of<br />
gold, with 20% to 80% silver. Orogenic mesothermal vein gold<br />
systems are characterized by abundant, typically iron-rich,<br />
hydrothermal carbonate alteration assemblages which spread into<br />
the host rock from the vein. They represent pulses of fluid which<br />
flowed along the hctudfault plane into the surrounding country<br />
lock with which they am not in chemical equilibrium, producing<br />
chemical reactions and the resultant alteration halo.