reading for friday: p.12-15 get computer accounts, buy...
TRANSCRIPT
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Announcements
Reading for Friday: p.12-15
Get computer accounts, buy hand lenses after lecture $7.53, UC Regents
First lab today
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Overview of next two weeks• Structure and composition of the Earth• Heat production and thermal gradients
in the Earth• Mechanisms for melt generation• What is a melt and how does it behave?
• Lab: Learn to identify and classify igneous rocks, minerals, and textures
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Structure of EarthSort of like an onion
Why do we care for Igneous Petrology?
Where are the igneous rocks?
How do we “know” this?
From Winter, Intro to Igneous and Metamorphic Petrology
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Seismic profile of the Earth
• Why do we need to use geophysics to look inside the Earth?
• S = shear wave– Not propagated
through liquid (why?)• P = compressional
– Slow down through liquid
• Slinky demoFrom Winter, Intro to Igneous and Metamorphic Petrology
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Earth’s interiorPeridotite (ultramafic)
Upper Mantle:Low Velocity Layer 60-220 km
410 km (olivine -> spinel)
Transition Zone: velocity increases rapidly
660 km spinel -> perovskite-type SiIV -> SiVI
Lower Mantle has more gradual velocity increase
From Winter, Intro to Igneous and Metamorphic Petrology
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The Earth’s InteriorThe Earth’s Interior
Core: Core: FeFe--Ni metallic alloyNi metallic alloy
Outer Core is liquidOuter Core is liquidNo SNo S--waveswaves
Inner Core is solidInner Core is solid
Why is the structure of the Why is the structure of the Earth important in igneous Earth important in igneous petrology?petrology?
From Winter, Intro to Igneous and Metamorphic Petrology
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The Upper Mantle and CrustCrust:Oceanic crust
Thin: 10 kmRelatively uniform
stratigraphy
Continental CrustThicker: 20-90 km
average ~35 kmHighly variable
composition– Average ~
granodioriteLithosphere = rigid
Asthenosphere = weaker zone
From Winter, Intro to Igneous and Metamorphic Petrology
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Compositional vs. PhysicalAnother diagram
http://volcano.und.edu/vwdocs/vwlessons/plate_tectonics/part1.html
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The crust/mantle boundary
• What does the lower crust and upper mantle look like?
• Any outcrops?• New project to
drill to the moho(IODP in Atlantic)
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How many stories tall is the lithosphere?
Information:Lithosphere = 30 km under oceansOne story = 3 m (about 10 feet)1 km = 1000 m
3x104 m = 1x104 = 10,000 stories !!!3 m
Lithosphere: 30 km 1000 m = 30000m = 3x104 m1 km
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Earth like an onion?Plate tectonics
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Bulk composition of the Earth• How do we
“know” this?
• What would bulk mantle look like?
• Average core composition?
Na, Mn, P
From Winter, Intro to Igneous and Metamorphic Petrology
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Meteorites as “average composition” of the Solar System
• Ordinary chondritesrepresent earliest, undifferentiated material
• Assume bulk Earth composition is same as bulk solar system composition
• Take away metallic part of ordinary chondrite ~ bulk mantle + crust
chondrule
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Formation of planets: differentiation of large bodies
Pallasite: core-mantle boundary of planetoid
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Summary of important points
•• Igneous rocks are everywhereIgneous rocks are everywhere•• Structure of Earth, especially crust and Structure of Earth, especially crust and
upper mantleupper mantle•• Bulk composition of Earth approximated Bulk composition of Earth approximated
by ordinary by ordinary chondriteschondrites
•• Rocks of the crust and mantle in labRocks of the crust and mantle in lab