Exam 1 Flashcards
(52 cards)
Petrology
Study of rocks using optical microscopy
Reasons why we study petrology
- Crust and mantle are igneous
- Most metallics ores are associated w/ igneous rocks and process
- Natural hazards
- All of terrestrial planets/moons have igneous crust
Exposed
- Volcanic: by volcanic eruptions
- Intrusive: exposed by uplift, erosion, glaciation
-intrusive igneous rocks are usually older than other formations
Melting
- Isothermal decomposition
- Add h20
- Add heat
Three broad environments
- Extrusive (volcanic)
- Intrusive (plutonic)
- Hypobyssal (shallow intrusive rocks )
Congruent melting
Melt w/ same composition as the source( melting 100%- liquid) usually never happens
Systems 1,2,3
- Open- transfer heat and matter across the boundary between the system and the surroundings
- Closed - transfer of heat m/y
- Isolated- no transfer of heat or matter ( not possible)
OIB
Ocean island basalt (alkali olivine basalt)
MORB
Mid ocean ridge basalt (tholeiite)
IAT
Island arc thoeliite
WPB
Within plate basalts (continental rift -highly alkaline )
Primary basalt vs. primitive basalt
Primary basalt: first formed (usually don’t erupt )
Primitive: most mafic that are erupted
Xenolith types
- Eucrites (gabbro): ca plag, augite, olivine
- Dunite and wehrlite: contain different proportion of mg rich olivine and diopside pyroxenes
- Lherzolites and harzburgites: mg olivine, diopside, mg rich orthopyrozene
- Garnet peridotite and elcogite: ca rich and ca poor pyroxene, olivine and rich garnet
Hasashi kono
-Believed tholeittic lavas- contain on,y 1 group xenoliths
-mildly alkaline basalts: groups 1 and 2 xenos
-Highly alkali basalts: group 1,2,3 xenos
-stronglyy si deficient basalt: group 1,2,3,4 xenos
I-type
Igneous source
- trondhjenite
S-type
Sedimentary source
- Granite
A-type
An orgenic , Alkalin
(Continental rifting)
M type
charnocite (metamorphic rocks)
Granite tends to be paraluminous
(Has alot of Alumnous ) S-type
Metaluminous
Biotite
hornblende
(pyroxene)
Peraluminous
Biotite
muscovite
garnet
cordierite
andaluite
Spinel
Peralkaline
annite-rich
biotite
Fe-rich amphibole
(arfredsonite, riebeckite, eg.)
fayalite
Melting (anatexis)
- Addition of h2o
- Decompression
- Heating
What is an Invariant in a one-component system?
Whenever three places coexist at equilibrium.