Test #1 Flashcards
Quartz
SiO2
Muscovite
KAl2(AlSi3O10)(OH)2
Orthoclase
(K-feldspar)
KAlSi3O8
Augite
(Ca,Mg,Fe,Na)(Mg,Fe,Al)(Si,Al)2O6
Biotite
K(Mg,Fe)3(AlSi3O10)(OH)2
Olivine
(Mg,Fe,Mn)SiO4
In what tectonic environments is magma formed? (7)
- Mid-oceanic ridges
- Intracontinental rifts
- Island arcs (convergent)
- Active continental margins
- Back arc basins (Japan)
- Ocean island basalts (hot spots)
- Miscellaneous oddities
How does the geothermal gradient vary by location?
Tectonically stable: <25°C/km
Oceanic trenches: 5-10°C/km
Mid-oceanic ridges & volcanically active areas:
_>_50°C/km
What is the geothermal gradient?
Temperature decreases with depth
How are C° and K related?
K=C°+273
How is heat transferred within the solid Earth? (3)
- conduction – transfer by molecular vibration
- convection – buoyancy-driven exchange of heat
- advection – passive heat transfer by motion of rock
What are the sources of heat within the Earth? (3)
- Residual heat from early accretion
- Crystallization of inner core
- Radioactive decay of U, Th, K, etc. (30-50% of heat reaching the surface comes from radioactive decay)
Types of pressure (4)
- Lithostatic – by overlying rocks; same in all directions; does not deform rocks
- Deviatoric – different pressures in different directions
- Hydrostatic – exerted by a column of water
- Fluid – exerted by film of fluid in pore spaces
Different units of pressure
SI unit: Pascal
1 bar = 0.987 atm = 14.5 psi
1 kbar = 1000 bars
1 bar = 105 Pa
1 kilobar = 0.1 GPa
How are pressure and depth related?
P = ϱ g h
P = pressure
ϱ (rho) = density
h = height
g = gravity
Characteristcs of the core
- Fe-Ni metallic alloy
- Outer core is liquid
- Inner core is solid
Characteristics of continental crust
- Felsic
- Thick, light (~35km avg. thickness)
- Highly variable composition
Characteristics of the mantle
- Ultramafic
Low velocity layer: 60-220 km; seismic waves slow down
410 km: olivine condenses to spinel structure
660 km: spinel structure condenses to perovskite structer
Lower mantle: gradual velocity increase
General characteristics of oceanic crust
- Mafic
- Dense & thin (<10 km thick)
- Relatively uniform
Plagioclase feldspar
Albite: NaAlSi3O8
Anorthite: CaAl2Si2O8
Bowen’s Reaction Series

Feldspar ternary diagram

Pyroxene quadrilateral

Pluton vs. Country Rock
- Pluton is intrusive
- Country rock is rock that was originally there
Tabular vs. non-tabular
Tabular plutons are “table”-like, cut across (think 3D)
Concordant vs. discordant plutons
- Concordant runs parallel to country rock
- Discordant cuts across country rock
Dikes vs. Sills

Xenolith
Fragment of country rock that is broken off and enclosed within magma chamber
Laccolith
Highly viscous lava, does not spread out like a sill

Lopolith
Dense mafic magma, causes basin floor to sag

Batholith
- Non-tabular
- Viscous lava
- Instrusive
- Exposed areal extent > 100 km2
Stock
- Non-tabular
- Viscous lava
- Instrusive
- Exposed areal extent < 100 km2
Epizone
Shallow level
Country rocks < 300°C
Mesozone
5-10 km
Country rocks 300-500°C
Country rocks are somewhat ductile at this depth; plutons may be syn- or post-tectonic; foliation may occur in plutons
Catazone
Deep, <10 km
Country rocks 450-600°C or higher
Catazonal plutons form easily (often concordant), ductile country rock–partial melting of country rock can occur
Diapir

How does magma displace solid country rock? (4)
- Doming: upward folding or faulting of overlying strata by magmatic pressure
- Wall-rock assimilaton: magma “melts” its way up
- Stoping: Brittle country rocks break off and fall into magma (xenoliths may be visible)
- Exploitation of shallow pre-existing open fractures
Composition of ultramafic magma
<45% SiO2
Very rich in Mg, Fe
Composition of mafic magma
SiO2 content of 45-52%
Rich in Mg, Ca, Fe
Composition of intermediate magma
SiO2 content of 52-65%
Na/Ca composition
Composition of felsic magma
SiO2 content of 65-75%
Rich in Al, Na, K
Viscosity
- Resistance to flow
- Increases w/Si-O & Al-O bonds
- Felsic–generally most viscous
Volatiles
(volatile components of magma)
H20, CO2
Volatiles can break down polymers & reduce viscosity
Mafic magmas: 0.5-1% volatiles
Felsic magmas: up to 5% volatiles
Shield Volcano
Very large landforms, caused by low viscosity (mafic) magma
Cinder cone
- De-gassed (therefore more dense) magma
- Often form on other types of volcanoes
Composite Volcano
- Tall
- Built up layers
- Often thick felsic magma
Lava dome
“Bubble”-shaped extrusion formed by highly viscous magma
Flood basalt
Plateau formed by basaltic eruption of very low viscosity lava
Plinian eruption
Pyroclastic eruption that produces very high ash plume
Pyroclastic flow
- Cloud of pyroclastic material and gases
- Extremely hot (400-800°C)
- Can move 50-200km/hr
Pyroclastic Deposit
- Poorly sorted
- Ash mixed with pumice & lithic fragments
Pyroclastic Textures
Pyroclasts/tephra: ash, lapilli, blocks, bombs
Tuff: pyroclastic rock consisting of glass shards, mineral grains, and rock fragments
Ash: pulverized rock & glass, glass shards
Caldera
Large pit formed by collapse after eruption
Phreatic eruption
Hot magma comes in contact with surface/groundwater; produces steam
Maar
Crater formed by deep phreatic explosion
Tuff ring
Basaltic magma reacts with shallow ground/surface water
Tuff cone
Smaller & steeper; less violent phreatic eruption
System
Portion of the universe that you wish to study
Natural systems tend toward states of minimum energy.
Energy States
Unstable
Stable: at rest in lowest energy state
Metastable: at rest in temporary low-energy “perch”
Gibbs Free Energy
A measure of chemical energy
G = H - T S
G = Gibbs Free Energy
H = Enthalpy (heat content)
T = Temperature in K
S = Entropy (degree of randomness in atomic arrangement)
Phase
Seperable portion of a system (ex: different minerals in a rock)
Reaction
Change in the nature or phase of a system
reactants = products
Must be balanced!
ΔG
If ΔG is negative, products are stable
If ΔG is positive, reactants are more stable
If ΔG is zero, the system is at equilibrium
Formula for determining G for P & T different from reference state
GT2P2= GT1P1 + V (P2 - P1) - S (T2 - T1)
Extensive Variables
Depend on quantity
- Mass
- Volume
- Free energy
Intensive Variables
Do not depend on size
- Pressure
- Temperature
- Density
- Molar volume
Augite
(Ca,Mg,Fe,Na)(Mg,Fe,Al)(Si,Al)2O6