iii. igneous rocks minerals crystallized from melts
DESCRIPTION
III. Igneous Rocks Minerals Crystallized from Melts. 1. The Rock Cycle 2. Formation of Igneous Rocks 3. Classification of Igneous Rocks 4. Igneous Rocks and Plate Tectonics. Geological Materials Transformation Processes. The Rock Cycle. Igneous Rock Solidification Magma - PowerPoint PPT PresentationTRANSCRIPT
III. Igneous RocksMinerals Crystallized from Melts
1. The Rock Cycle
2. Formation of Igneous Rocks
3. Classification of Igneous Rocks
4. Igneous Rocks and Plate Tectonics
The Rock Cycle
Igneous Rock
Solidification
Magma
Partial Melting
Mantle Rock Fig 3.1
Geological Materials
Transformation Processes
See Kehew, Fig. 1-6
Partial Melting and MagmaE.g., partial melting results in Silica enrichment
Partial Melting MagmaEnriched: O, Si, Al, Na, K, Depleted: Ca, Fe, Mg Poor in: O, Si, Al, Na, K, (<50%) Rich in: Ca, Fe, Mg (>50% wt.)
See Kehew, Fig 3-6
Formation of Magma
How are rocks melted? 1. Heating ■ 2. Depressurization 3. Increase water content 4. Increased silica content
Where do rocks melt? Subduction zones (Silicic
and Intermediate) Mantle Plumes (“Hot Spots”) not only at
Divergent
Boundaries
MaficSee Kehew, Fig 3-6
Hot andHigh Pressure
Hot andLow Pressure
See Kehew Fig. 3-8
Solidification of Melts
• Magma, Intruded or Extruded,• Solidifies (crystallizes) to form
• Intrusive or Extrusive • Igneous Rocks
Fig 3.12, 3.13See Kehew, Fig 3-6
Intrusive vs. Extrusive (Silicic Rocks)
Silicic (a.k.a, felsic) Magmas Cool (<700oC) Viscous (sticky, doesn’t flow easily) Gaseous (steam of H2O and C02)
Silicic Rocks Usually intrusive, course-grained, Silicic (Granite) to Intermediate
(Diorite) rock forms plutons If extrusive, fine-grained rocks
formed by explosive volcanoesRhyolite or Andesite Volcanoes
Also injects surrounding rocks with silica laden steam
See Kehew, Fig 3-40
Intrusive Igneous RockE.g., Granite (Silicic, Phaneritic):
Crystallized (Solidified) Silicic Magma Poor in: Fe, Mg, Ca, (<20%) Rich in: Silica (>70%)
Quartz
Na Plagioclase
Biotite
Composite Volcanoes Silicic magma High-viscosity Gaseous Explosive
eruptions Steep sloped,
cone shaped volcanoes
Extrusive vs. Intrusive (Mafic Rocks)
Mafic Magmas Hot (>1000oC) Non-Viscous (runny, flows easily) “Dry” (no H2O or C02)
Mafic Rocks Usually Extrusive, Fine-grained,
Mafic (Basalt) rock forms oceanic crust, Shield Volcanoes and Basalt Floods
If Intrusive, course-grained mafic rocks are formed Gabbro.
If intrusive, Dikes and Sills more common
See Kehew, Fig 3-40
E.g., Mafic Volcanism, Hawaii
Mantle Hot Spot Volcano
See Kehew, 3-8
Hawaii
10.3 12.0
20.6
Midway 27.2 19.9 43.4
42.4
48.1 55.2
56.2 59.6
0-5
Current PlateMotion
HawaiiA long chain of inactive volcanoes Island ages, millions of years
Shield Volcanoes
Mafic Magma Low-viscosity Non-explosive eruptions Gentle slopes Covering large areas
Types of Eruptions (Mafic Volc.)
Types of Eruptions Lava floods Lava fountains Fissure eruptions
Rock Textures (Table 3-1)
Aphanitic Porphyritic Vesicular Glassy (Obsidian)
Surface Textures (Extrusive, Mafic Rocks)
Ahah (Rubbley) Mostly solid when
flowing Pahoehoe (Ropey)
mostly liquid when flowing)
See Kehew, Fig 3-9, 3-10
Volcanic Hazards Relative Hazard (see Kehew, Fig. 3-30, 31)
based on Type of volcano Active Vents Earthquakes Calderas Historical Flows Rift Zones Slopes
Mafic Sill: Intruded between layers Mafic magma is less
viscous and hotter so Does not form plutons
but Cuts along layers (Sills)
or even across layers (Dikes) Also Baked Zones
of adjacent country rock and Chill Zones within the intrusion
Igneous Rock ClassificationIntrusive (Plutonic)
Extrusive (Volcanic)
See Kehew, Fig. 3-5
Min
eral
Per
cen
tag
e
Continental Crust Oceanic Mantle Crust
Igneous Rocks and Silicates
The
Igneous Rock Classification
parallels the
systematic
Silicate Mineral Classification
Frame- Double Single Iso. work Sheet Chain Chain
Fig
. 3-6
Min
eral
Per
cen
tag
e
Igneous Rock Classification Silicic Intermediate Mafic
Granite Diorite Gabbro
Rhyolite Andesite Basalt
(Porphyritic)
Intr
usi
veE
xtru
sive
1200
oC
1000
o
Bowen’s Reaction SeriesTwo series of minerals formed during crystallization of magma
Intrus. Extrus.
Gabbro Basalt
Diorite Andesite
Granite Rhyolite
Low Silica Magma
High Silica Magma
Fra
me-
D
oubl
e
S
ingl
e
Isol
ated
wor
k
S
heet
Cha
in
Cha
in
Temperature ofCrystallization
750
o