Chunky Iggy Rocks. All igneous rocks are formed from liquid rock known as __________? O Magma.
Magma, Rocks Classification & Textures
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Transcript of Magma, Rocks Classification & Textures
Magma, Rocks Classification & Textures
MAGMA
MAGMA
• Larutan silikat yang sangat panas• Mengandung oksida, sulfida serta
volatiles (CO2, sulfur, chlorine, fluorin, boron dll)
• Temperatur antara 600°C (magma asam) sampai 1250°C (magma basa)
JENIS KONVERGEN
Plate Tectonic - Igneous Genesis
? ???
600 km
400
200 km
Continental Crust
Oceanic Crust
Lithospheric Mantle
Sub-lithospheric Mantle
Source of Melts
15 3 46 7 2
Environments of Magma Formation
Environments of Magma Formation
Stages in ascent
• EruptionEruption
• (Fragmentation)(Fragmentation)
• VesiculationVesiculation
• Renewed ascent Renewed ascent
• StorageStorage
– mixingmixing
– assimilationassimilation
– crystallizationcrystallization
• Buoyant ascentBuoyant ascent
• Partial meltingPartial melting
The Earth’s InteriorThe Earth’s Interior
Crust:Crust:Granite/Andesite (felsic)Granite/Andesite (felsic)
Mantle:Mantle:Peridotite (ultramafic)Peridotite (ultramafic)
Core:Core:Metal alloy/liquidMetal alloy/liquid
6370
5145
2898
660
410
60220
Crust
MantleMantle
CoreCore
Upper Mantle
Transition Zone
Inner Core
Depth (km)
LowerMantle
(solid)
OuterCore
(liquid)
Figure 1-5. Relative atomic abundances of the seven most common elements that comprise 97% of the Earth's mass. An Introduction to Igneous and Metamorphic Petrology, by John Winter , Prentice Hall.
O50.7%
Mg15.3%
Fe15.2%
Si14.4%
S3.0%
Al1.4%
Ca1.0%
Most important elementsMost important elements
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)
Urutan pembekuan magma
• Pada pembekuan magma, pada awalnya mineral yang terbentuk adalah yang anhydrous (tidak mengandung air) tidak mengandung gugus OH, disebut mineral pyrogenetik.
• Cairan selanjutnya akan lebih banyak mengandung komponen gas dan terbentuk mineral-mineral yang mengandung gugusan hydroksil (OH), disebut mineral hydratogenetik.
Diferensiasi Magma
• Proses diferensiasi meliputi semua kegiatan yang mengakibatkan suatu jenis magma induk yang semula relatif homogen terpecah-pecah menjadi beberapa bagian atau fraksi dengan komposisi yang berbeda-beda. Hal ini disebabkan karena migrasi ion atau molekul dalam larutan magma karena adanya perubahan temperatur dan tekanan. Yang pada akhirnya akan membentuk berbagai jenis batuan beku dengan komposisi yang berbeda-beda pula.
Bowen reaction series
DIAGRAM FASE
• Fase : padat, cair, gas
• Diagram fase : menggambarkan kondisi magma pada kondisi P & T tertentu
• Parameter penting dalam sistem magma : fase, komponen, variabel intensif
DIAGRAM fASE
• fase : padat, cair• komponen : komponen terkecil yang
diperlukan utk pembentukan fase-fase
• dalam sistem (OH, H2O, MgO, NaAlSi3O8, dll)
•
• variabel intensif : temperatur dan tekanan, jumlah komponen
DIAGRAM FASE
• Rumus fase : F = C – P + 2
• F : degree of freedom : jumlah kondisi minimum
• C : jumlah komponen;
• P : jumlah fase
• contoh utk air – es ------ C = 1 (H2O) ; P = 2 (es dan air)
• F = C – P + 2 ---- F = 1 – 2 + 2 = 1 (unary system)
SISTEM 1 KOMPONEN
SISTEM 2 KOMPONEN (BINER) DGN TITIK EUTEKTIK
h : titik eutektik; titik terendah fase cair ; kondisi terbentuknya 2 komponen
SISTEM 2 KOMPONEN SOLID - SOLUTION
SISTEM 2 KOMPONEN INCONGRUENT MELTING
Why storage?
denser
stronger
crus
tcr
ust
Why do some magmas stall and pond in chambers during Why do some magmas stall and pond in chambers during ascent?ascent?
Fractional Crystallization
http://www.geolsoc.org.uk/webdav/site/GSL/shared/images/geoscientist/Geoscientist%2019.2/7%20Volcano%20and%20magma%20chamber%20James%20Island2resized.jpg
Processes during storage in magma chambers
http://www.geolsoc.org.uk/webdav/site/GSL/shared/images/geoscientist/Geoscientist%2019.2/7%20Volcano%20and%20magma%20chamber%20James%20Island2resized.jpg
Gravity settling
Processes during storage in magma chambers
Gravity settling and cumulates
http://www.geol.lsu.edu/henry/Geology3041/lectures/12LayeredMafic/Fig12-15.jpg
Buoyancy, sinking: Stoke’s Buoyancy, sinking: Stoke’s LawLaw
VV = the settling velocity (cm/sec)= the settling velocity (cm/sec)
gg = the acceleration due to gravity (980 cm/sec= the acceleration due to gravity (980 cm/sec22) )
r r = the = the radiusradius of a spherical particle (cm) of a spherical particle (cm)
ss = the density of the solid spherical particle = the density of the solid spherical particle
(g/cm(g/cm33))
ll = the density of the liquid (g/cm= the density of the liquid (g/cm33))
= the viscosity of the liquid (1 c/cm sec = 1 = the viscosity of the liquid (1 c/cm sec = 1 poise)poise)
V2gr ( )
9
2
s l
Olivine in basaltOlivine in basalt
Olivine (Olivine (ss = 3.3 g/cm = 3.3 g/cm33, r = 0.1 cm) , r = 0.1 cm)
Basaltic liquid (Basaltic liquid (ll = 2.65 g/cm = 2.65 g/cm33, , = 1000 poise) = 1000 poise)
V = 2·980·0.1V = 2·980·0.12 2 (3.3-2.65)/9·1000 = 0.0013 cm/sec(3.3-2.65)/9·1000 = 0.0013 cm/sec
that’s ~1m per daythat’s ~1m per day
Sinking olivine in basaltSinking olivine in basalt
Rhyolitic meltRhyolitic melt = 10= 1077 poise and poise and ll = 2.3 g/cm = 2.3 g/cm33
hornblende crystal (hornblende crystal (ss = 3.2 g/cm = 3.2 g/cm33, r = 0.1 cm) , r = 0.1 cm) V = 2 x 10V = 2 x 10-7-7 cm/sec, or 6 cm/year cm/sec, or 6 cm/year
feldspars (feldspars (ll = 2.7 g/cm = 2.7 g/cm33) ) V = 2 cm/yearV = 2 cm/year = 200 m in the 10= 200 m in the 1044 years that a stock might cool years that a stock might cool If 0.5 cm in radius (1 cm diameter) settle at 0.65 If 0.5 cm in radius (1 cm diameter) settle at 0.65
meters/year, or 6.5 km in 10meters/year, or 6.5 km in 1044 year cooling of stock year cooling of stock
Sinking x’tal in rhyoliteSinking x’tal in rhyolite
IGNEOUS ROCKS CLASSIFICATION
Ternary diagramsTernary diagrams
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
YZ
Incr
%X
Incr %Y Incr %Z
30 20 10
10
20
30
10
20
30%Z
20
10
30%X
A%Y
%Z
Know how to classify a rockKnow how to classify a rock
Volcanic rocks: aphanitic
Ultra-mafic rocks & felsic vs. mafic
Classification of Igneous Rocks
Figure 2-2. A classification of the phaneritic igneous rocks. b. Gabbroic rocks. c. Ultramafic rocks. After IUGS.
Plagioclase
OlivinePyroxene
Olivine gabbro
Plagioclase-bearing ultramafic rocks
90
(b)
Anorthosite
OlivineOlivine
ClinopyroxeneClinopyroxeneOrthopyroxeneOrthopyroxene
LherzoliteLherzoliteH
arzb
urgi
te
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)ite
Phono-tephrite
13
Tephri-phonolite
Trachy-andesite
Phonolite
Trachyte
Basaltic trachy- andesite
Trachydacite
Trachy-basalt
BasalticAndesite
Andesite
Dacite
Rhyolite
TephriteBasanite
63ULTRABASIC BASIC INTERMEDIATE ACIDIC
wt% SiO2
Wt.
% N
a2O
+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
TuffLapilli-stone
(b)
30 30
7070PyroclasticBreccia or
Agglomerate
Lapilli (2-64 mm)
TEXTURES IN IGNEOUS ROCKS
Textures: result of nucleation+growth
Grain size
Fast growth
a
Ocean Drilling ProgramOcean Drilling Program
Crystal zoning
Crystal shape
Growth order
Quartz - feldspar intergrowth
Remelting
Matrix texture
Twinning
Replacements
North CarolinaNorth CarolinaState UniversityState University Smith CollegeSmith College