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Metamorphic Rocks 1:

Metamorphic Rocks 1:

Metamorphic Rocks 1:. Description and Classification Introduction to Lab MR-1 Nesse Ch. 11, p. 194-200 Lab Manual: Introduction p. 30-49 Lab MR-1 p. 50-52. Rock-Mineral Associations?. mineral stability is a function of:. pressure ( P ) temperature ( T ) composition ( X ).

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376 views • 37 slides
Lecture 9: Rocks and Minerals

Lecture 9: Rocks and Minerals

Lecture 9: Rocks and Minerals. References: Principles and applications of Geochemistry (Ch. 7 & 8) Igneous Petrogenesis (Ch. 2). How are rocks formed: the rock cycle. www.geolsoc.org.uk. Granite: intrusive igneous rock. quartz. hornblende. feldspar. What defines a mineral?.

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615 views • 25 slides
Lecture 3: Rocks and Minerals

Lecture 3: Rocks and Minerals

Lecture 3: Rocks and Minerals. References: Principles and applications of Geochemistry (Ch. 7 & 8) Igneous Petrogenesis (Ch. 2). How are rocks formed: the rock cycle. www.geolsoc.org.uk. Granite: intrusive igneous rock. quartz. hornblende. feldspar. What defines a mineral?.

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623 views • 25 slides
Mantle composition

Mantle composition

Mantle composition. 1800s meteorites contain similar minerals to terrestrial rocks Hypothesis that meteorites come from asteroid belt and originate from a single planet with metallic core a silicate mantle and crust Earth must be similar. Mantle composition.

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371 views • 24 slides
Ralph Pudritz, Origins Institute, McMaster

Ralph Pudritz, Origins Institute, McMaster

The Search for Life in Exoplanetary Systems. Ralph Pudritz, Origins Institute, McMaster. (LRP 2010 Toronto Town Hall, March 17, 2010). Astrobiology- the search for life. Three scientific revolutions driving the search for life:

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Internal Structure of the Earth : geology's most wildly speculative topic

Internal Structure of the Earth : geology's most wildly speculative topic

Internal Structure of the Earth : geology's most wildly speculative topic.

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230 views • 11 slides
1. A bulk composition of X cools to the liquidus, at which point An crystallizes.

1. A bulk composition of X cools to the liquidus, at which point An crystallizes.

1. A bulk composition of X cools to the liquidus, at which point An crystallizes. 2. Continued crystallization of An causes liquid composition to move toward Di.

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78 views • 1 slides

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