The Goldschmidt System in Geology

 
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Chemistry of the Earth
Bulk composition comparable to Chondrites
 
Chondrites are one of the
stony meteorites,  formed
when various types of dust
and small grains that were
present in the early solar
system accreted to form
primitive asteroids
 
Chondrites are the most
common type of meteorite
accounting for approximately
82% of all meteorites
The Goldschmidt Classification of Elements
 
Swedish born mineralogist considered
to be one of the founders of modern
geochemistry and crystal chemistry
 
Chemical elements on the periodic table
are classified into groups according to
their preferred host phases
 
4 groups are recognised: Lithophile,
Siderophile, Chalcophile and Atmophile
 
Victor Moritz Goldschmidt
1888 - 1947
The Goldschmidt Classification of Elements
Lithophile Elements - Concentrated in the Crust
 
Lithophile (rock loving) elements are found close to the Earth’s surface as they
combine readily with oxygen, forming compounds that do not sink into the core.
 
The lithophile elements include:
 
Aluminium
Calcium
Potassium
Magnesium
Sodium
Oxygen
Silicon
Titanium
Elemental Composition of the Earth’s Crust
 
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:
 
Oxygen
Silicon
Aluminium
Iron
Calcium
Sodium
Potassium
Magnesium
Lithophile Elements – Concentrated in the Crust
 
Found in the silicate minerals which make
up 93% of the crust by mass and constitute
the common rock-forming minerals
 
Quartz
Orthoclase Feldspar
Plagioclase Feldspar
Biotite Mica
Muscovite Mica
Hornblende (Amphibole)
Augite (Pyroxene)
Olivine
Garnet
Clay Minerals (Kaolinite)
 
Siderophile Elements – Concentrated in the Core
 
Siderophile (iron-loving) elements
High density metals
Tend to sink into the Earth’s core
Do not combine with oxygen
Dissolve readily in iron as solid solutions or in the molten state
The siderophile elements include
 
Gold
Iridium
Iron
Molybdenum
Nickel
Platinum
    Chalcophile Elements – Trace amounts in the Crust
 
Chalcophile (ore-loving) elements
Combine readily with sulphur
Form compounds that do not sink to the core
Make up just 0.046% of crust by mass (More concentrated in mineral veins)
Chalcophile elements include
 
Arsenic
Cadmium
Copper
Lead
Silver
Sulphur
Tin
Zinc
Atmophile 
Elements
 – Concentrated in the
Atmosphere and Hydrosphere
 
Atmophile  (atmosphere-loving) elements
Also known as volatile elements
Occur in gases and liquids close to the Earth’s surface
The atmophile elements are
 
Carbon
Hydrogen
Nitrogen
Argon
Helium
Neon
Krypton
Xenon
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Explore the Goldschmidt System in geology, which classifies chemical elements based on their preferred host phases. Learn about lithophile elements concentrated in the Earth's crust and the elemental composition of the crust. Discover the significance of chondrites in meteorites and the foundational work of Victor Moritz Goldschmidt in geochemistry and crystal chemistry.

  • Geology
  • Goldschmidt System
  • Lithophile Elements
  • Elemental Composition
  • Chondrites

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  1. AS-A level Geology The Goldschmidt System Click anywhere on the screen to move on. AS-A level Geology

  2. Chemistry of the Earth AS-A level Geology

  3. Bulk composition comparable to Chondrites Chondrites are one of the stony meteorites, formed when various types of dust and small grains that were present in the early solar system accreted to form primitive asteroids Chondrites are the most common type of meteorite accounting for approximately 82% of all meteorites AS-A level Geology

  4. The Goldschmidt Classification of Elements Swedish born mineralogist considered to be one of the founders of modern geochemistry and crystal chemistry Chemical elements on the periodic table are classified into groups according to their preferred host phases 4 groups are recognised: Lithophile, Siderophile, Chalcophile and Atmophile Victor Moritz Goldschmidt 1888 - 1947 AS-A level Geology

  5. The Goldschmidt Classification of Elements AS-A level Geology

  6. Lithophile Elements - Concentrated in the Crust Lithophile (rock loving) elements are found close to the Earth s surface as they combine readily with oxygen, forming compounds that do not sink into the core. The lithophile elements include: Aluminium Calcium Potassium Magnesium Sodium Oxygen Silicon Titanium AS-A level Geology

  7. Elemental Composition of the Earths Crust Elemental Composition of the Earth s Crust 99% of the earth s crust by weight is made up of just eight elements: Oxygen Silicon Aluminium Iron Calcium Sodium Potassium Magnesium AS-A level Geology

  8. Lithophile Elements Concentrated in the Crust Found in the silicate minerals which make up 93% of the crust by mass and constitute the common rock-forming minerals Quartz Orthoclase Feldspar Plagioclase Feldspar Biotite Mica Muscovite Mica Hornblende (Amphibole) Augite (Pyroxene) Olivine Garnet Clay Minerals (Kaolinite) AS-A level Geology

  9. Siderophile Elements Concentrated in the Core Siderophile (iron-loving) elements High density metals Tend to sink into the Earth s core Do not combine with oxygen Dissolve readily in iron as solid solutions or in the molten state The siderophile elements include Gold Iridium Iron Molybdenum Nickel Platinum AS-A level Geology

  10. Chalcophile Elements Trace amounts in the Crust Chalcophile (ore-loving) elements Combine readily with sulphur Form compounds that do not sink to the core Make up just 0.046% of crust by mass (More concentrated in mineral veins) Chalcophile elements include Arsenic Cadmium Copper Lead Silver Sulphur Tin Zinc AS-A level Geology

  11. Atmophile Elements Concentrated in the Atmosphere and Hydrosphere Atmophile (atmosphere-loving) elements Also known as volatile elements Occur in gases and liquids close to the Earth s surface The atmophile elements are Carbon Hydrogen Nitrogen Argon Helium Neon Krypton Xenon AS-A level Geology

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