continued intro classification. updates lab starts this week monday 9.30-12.20 lab, wednesday...
DESCRIPTION
The Pressure Gradient P increases = gh Nearly linear through mantle –~ 30 MPa/km – 1 GPa at base of ave crust Core: incr. more rapidly since alloy more dense Depth (km) Pressure (GPa) 40 Mantle Core Figure 1-8. Pressure variation with depth. From Dziewonski and Anderson (1981). Phys. Earth Planet. Int., 25, © Elsevier Science.TRANSCRIPT
Continued intro & classification
7773696561575349
52
Basalt
454137
45
Picro-basalt1
3
5
7
9
11
(Foid)itePhono-tephrite
13Tephri-phonolite
Trachy-andesite
Phonolite
Trachyte
Basaltic trachy- andesite
Trachydacite
Trachy-basalt
BasalticAndesite
Andesite
Dacite
Rhyolite
TephriteBasanite
63ULTRABASIC BASIC INTERMEDIATE ACIDIC
wt% SiO2
Wt.% Na
2O+K
2O
Updates
•Lab starts this week•Monday 9.30-12.20 lab, •Wednesday 2.30-5.30 lab
Today’s topics:1a. Heat, pressure and the geotherm1b. Geotherm and melting1c. Different ways to melt2. Classification of igneous rocks
The Pressure Gradient
• P increases = gh• Nearly linear through mantle
– ~ 30 MPa/km 1 GPa at base of ave
crust• Core: incr. more rapidly
since alloy more dense
1010 2020 303000
10001000
20002000
30003000
40004000
50005000
60006000D
epth
(km
)D
epth
(km
)
Pressure (GPa)Pressure (GPa)4040
Mantle
Core
Figure 1-8. Pressure variation with depth. From Dziewonski and Anderson (1981). Phys. Earth Planet. Int., 25, 297-356. © Elsevier Science.
Heat
Heat Sources Heat Sources in the Earthin the Earth
The Geothermal GradientCrust
Mantle
OuterCore
Temperature(K)
0 5 10
1000
2000
3000
4000
5000
6000
Dep
th (k
m) S waves
P waves
InnerCore
Lithosphere
Astheno-sphere
Solid
Liquid
Meso-sphere
S waves
Rocks at different depth: change in P & T: Phase
changeT T
P P
Atoms have a “choice” as to how they want to arrange
themselves in a phase
Plate Tectonic - Igneous Genesis
? ???
600 km
400
200 kmContinental CrustOceanic CrustLithospheric MantleSub-lithospheric Mantle
Source of Melts
15 3 46 7 2
Geotherm and solidus: how to melt
Processes That Form Magma
Processes that form magma and rock
Environments of Magma Formation
Environments of Magma Formation
Environments of Magma Formation
Environments of Magma Formation
Environments of Magma Formation
Partial Melting: The Origin of Basalt and Granite
Asthenosphere40% Silica
Melting
Basaltic magma = 50% silica (1100o C)
Forms the rock basalt
Partial Melting: The Origin of Basalt and Granite
Continental Crust(Mainly low melting point minerals such as quartz, feldspar, mica)
Melting
Granitic magma ~ 70% silica (700-900o C)
Forms granite (a mixture of quartz and feldspar)
Classification of Igneous Rocks
Figure 2-1a. Method #1 for plotting a point with the components: 70% X, 20% Y, and 10% Z on triangular diagrams. An Introduction to Igneous and Metamorphic Petrology, John Winter, Prentice Hall.
X
YZIncr %X
Incr %Y
Incr %Z
30 20 10
10
2030
10
20
30%Z
20
10
30%X
A%Y
%Z
Classification of Igneous Rocks
Figure 2-1b. Method #2 for plotting a point with the components: 70% X, 20% Y, and 10% Z on triangular diagrams. An Introduction to Igneous and Metamorphic Petrology, John Winter, Prentice Hall.
Y
X
Z
70
67
A
100
0
%X
Classification of Igneous RocksFigure 2-2. A classification of the phaneritic igneous rocks. b. Gabbroic rocks. c. Ultramafic rocks. After IUGS.
Plagioclase
OlivinePyroxene
Gabbro
Troctolite
Olivine gabbro
Plagioclase-bearing ultramafic rocks
90
(b)
Anorthosite
OlivineOlivine
ClinopyroxeneClinopyroxeneOrthopyroxeneOrthopyroxene
LherzoliteLherzoliteHa
rzbu
rgite
Wehrlite
Websterite
OrthopyroxeniteOrthopyroxenite
ClinopyroxeniteClinopyroxenite
Olivine Websterite
PeridotitesPeridotites
PyroxenitesPyroxenites
90
40
10
10
DuniteDunite
(c)
Classification of Igneous Rocks
Figure 2-4. A chemical classification of volcanics based on total alkalis vs. silica. After Le Bas et al. (1986) J. Petrol., 27, 745-750. Oxford University Press.
7773696561575349
52
Basalt
454137
45
Picro-basalt1
3
5
7
9
11
(Foid)itePhono-tephrite
13Tephri-phonolite
Trachy-andesite
Phonolite
Trachyte
Basaltic trachy- andesite
Trachydacite
Trachy-basalt
BasalticAndesite
Andesite
Dacite
Rhyolite
TephriteBasanite
63ULTRABASIC BASIC INTERMEDIATE ACIDIC
wt% SiO2
Wt.% Na
2O+K
2O
Classification of Igneous Rocks
Figure 2-5. Classification of the pyroclastic rocks. a. Based on type of material. After Pettijohn (1975) Sedimentary Rocks, Harper & Row, and Schmid (1981) Geology, 9, 40-43. b. Based on the size of the material. After Fisher (1966) Earth Sci. Rev., 1, 287-298.
Glass
Rock Fragments Crystals
VitricTuff
LithicTuff
CrystalTuff
(a)
Ash (< 2 mm)
Blocks and Bombs(> 64 mm)
LapilliTuff
Lapilli -TuffBreccia
Tuff Lapilli-stone
(b)
30 30
7070PyroclasticBreccia or
Agglomerate
Lapilli (2-64 mm)