@hamburger,
The term "Dacite" is an igneous rock classification based on a system called the QAPF system. Igneous rocks are classified , simply, based on the percentages of free silica(Q) they contain (IE quartz), the chemical makeup of the feldspars (AP)within the mix (plagioclase is a calcium rich and high temperature feldspar, while orthoclase is a sodium rich and hence, COOLER feldspar), and lastly the amount of fwldspathoids (F) , the F, or Foid minerals are similar to feldspars but contain much less silica and more of things like aluminum and magnesium. Then on top, each of the rocks are classed according to grain size (Small grains are explosives and large grains are deep rocks).
SO the classification of a dacite, by the QAPF system ,means that this rock has a small grain appearance and a chemical makeup similar to granites and diorites, except, unlike granites, these are mostly primary melted rocks .
What the petrologist is looking at is the chemical and physical makeup of these rock types in a mantle mix. That can tell us how deep it was emplaced or its methodof crystrallization.
Dacites are often good metal ore producing zones so we often look for them as a princip[al ore carrier, especially if these rocks are emplaced right along side a sedimentary rock body.
anybody awake yet?