Prof. Gorring
GEOS 112 PHYSICAL GEOLOGY
Sept. 9, 1998
Minerals & Rock Cycle
1. MINERALS
- Mineral- naturally occurring, solid crystalline,
inorganic, and specific chemical composition.
- Crystal growth, crystallization, precipitation.
- Atomic Structure
-
Atoms = smallest unit of an element that retains elemental
properties.
-
Protons (atomic #) + Neutrons = Nucleus (atomic mass);
Isotopes. Electrons, Shell Structure, Ions (cations, anions; size); Ion
Complexes; Periodic Chart.
- Chemical Bonds:
Ionic- electrical attraction bewteen cations
and anions (Na+ and Cl-). Most
common in minerals.
Covalent- electrons are shared in outer shell.
Stronger than ionic (C-diamond).
- Rock-forming minerals (~30 out of thousands of known
minerals)
-
Silicates- SiO44-
tetrahedron; bonds with cations or share O with other tetrahedra
-
Isolated
-
Rings
-
Single-chains Cation substitution
-
Double-chains
-
Sheets
-
3D networks
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Carbonates- CO32-
(calcite, dolomite)
-
Sulfates- SO42-
(anhydrite, gypsum)
-
Halides- Cl-, F-,
Br-, I- (halite)
-
Oxides and Hydroxides- O2-
and OH- (hematite, magnetite,
brucite)
-
Native elements- (gold, copper, sulfur, carbon - [polymorphism])
-
Sulfides- S2-
(pyrite, galena)
2. THE ROCK CYCLE
The Rock Cycle- interrelated set of
geologic processes that link the three rock types. Ultimately driven
by plate tectonics and atmospheric processes.
-
Igneous Rocks-
crystallization of magma (700°-1100°C). Intrusive and Extrusive
types.
-
Sedimentary Rocks - lithification of sediments
in to layers called "beds" or bedding. Sediments produced by weathering
and erosion; Clastic, Biochemical, and Chemical types. Transportation,
deposition, lithification (compaction, cementation)
Metamorphic Rocks - solid state change
at high T (250°-700°C) and P. Regional, Contact metamorphism;
Foliated and non-foliated types.