Recap Qs: What are the two most abundant elements in crustal rocks - PowerPoint PPT Presentation

1 / 14
About This Presentation
Title:

Recap Qs: What are the two most abundant elements in crustal rocks

Description:

Why can mica be easily splitted into thin sheets ? A. mica ... Rocks formed from magma at depth = intrusive, or plutonic rocks. Classification of Igneous rocks: ... – PowerPoint PPT presentation

Number of Views:61
Avg rating:3.0/5.0
Slides: 15
Provided by: mian4
Category:

less

Transcript and Presenter's Notes

Title: Recap Qs: What are the two most abundant elements in crustal rocks


1
Recap Qs What are the two most abundant
elements in crustal rocks?
  • A. Potassum and Sodium
  • B. Calsum and Aluminum
  • C. Copper and Iron
  • D. Silicon and Oxygen

2
Recap Qs Why can mica be easily splitted into
thin sheets ?
  • A. mica is a silicate mineral.
  • B. mica is soft.
  • C. mica has a sheet silicate structure.
  • D. mica has a single-chain silicate structure.

3
Principles of Geology
  • Chapter 4 Igneous Rocks

Mian Liu 2007
4
Igneous Rocks
  • Name from latin ignis, or fire
  • Formed from cooling and solidification
    (crystallization) of magma.

5
General characteristics of magma
  • General characteristic of magma
  • Rocks formed from lava extrusive, or volcanic
    rocks
  • Rocks formed from magma at depth intrusive, or
    plutonic rocks

6
Classification of Igneous rocks
  • Texture
  • Mineral composition

7
  • Texture overall appearance of rocks based on
    size, shape, arrangement of their interlocking
    cystals.
  • Reflect the environment in which the rocks formed.

8
Factors contribute to the textures of igneous
rocks
  • Magma cooling rate
  • Amount of silica in the magma
  • Amount of dissolved gas in the magma

9
Igneous Textures
  • Aphanitic (fine-grained)
  • Phaneritic (coarse-grained)
  • Pegmatic (exceptionally coarse grained)
  • Porphyritic (phenocrysts goundmass)
  • Glassy
  • Pyroclastic (associated with volcanic eruption)

10
Naming Igneous Rocks
  • Texture
  • Phaneritic (intrusive)
  • Aphanitic (extrusive)
  • Composition
  • Ultramafic
  • Mafic
  • Intermediate
  • Felsic

11
Magma generation
  • Increase temperature
  • Reduce pressure
  • Add water and other volatiles

12
Temperature in Earths interior
13
Pressure-release partial melting
Partial melting starts
14
Assimilation, magma mixing, and magmatic
differentiation
Write a Comment
User Comments (0)
About PowerShow.com