| . |
Week 3: Jan 24-28
-
Review of some important igneous minerals
-
elements/ions in the crust
-
coordination of ions
-
silicates
-
orthosilicates
-
sorosilicates
-
cyclosilicates
-
inosilicates
-
phyllosilicates
-
tectosilicates
-
silica minerals
-
high quartz
-
low quartz
-
cristobalite
-
tridymite
-
coesite
-
stishovite
-
physical properties of quartz
-
feldspars
-
comparison of structure of feldspar to quartz
-
K-feldpspar, albite and anorthite
-
pyroxenes
-
olivine
-
feldspathoids
-
amphiboles
-
micas
-
Fe-Ti oxides
-
Classification of igneous rocks
-
fundamental division based on texture: plutonic
vs. volcanic
-
plutonic rock classification based on mineralogy
(IUGS or Streckeisen classification)
-
M<90, QAPF diagram
-
M>90, olivine-cpx-opx diagram
-
gabbroic rocks
-
problem with IUGS volcanic rock classification
-
Le Bas chemical classification of volcanic
rocks
-
Classification of volcanic rocks in the field
-
classification schemes based on chemistry
-
based on silica content (acid, intermediate,
basic, ultrabasic)
-
based on silica saturation (oversaturated,
saturated, undersaturated)
-
based on alumina saturation (peraluminous,
metaluminous, peralkaline)
-
Rock suite classifications
-
variation diagrams
-
Harker diagrams
-
Peacock "alkali-lime index"
-
subalkaline and alkaline suites (SiO2 vs alkalis
plot)
-
tholeiitic vs.calcalkaline suites (AFM diagram)
-
important conclusions from these diagrams
-
variations are not random
-
suites seem to correlate with general tectonic
setting
Petrology
homepage |
Saint Louis University
| Earth & Atmospheric Sciences
|