Clastic Sedimentary Rocks Derived from the Mechanical Breakup and Redeposition of Older Rocks.

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Clastic Sedimentary Rocks Derived from the Mechanical Breakup and Redeposition of Older Rocks

Transcript of Clastic Sedimentary Rocks Derived from the Mechanical Breakup and Redeposition of Older Rocks.

Page 1: Clastic Sedimentary Rocks Derived from the Mechanical Breakup and Redeposition of Older Rocks.

Clastic Sedimentary Rocks

Derived from the Mechanical Breakup and Redeposition of Older Rocks

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Clastic Rocks

Classified by:• Grain Size • Grain Composition • Texture

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The Wentworth Scale

• Phi (φ) = -log2(Diameter in mm)

• Best way to remember:–1mm: φ = 0–φ increases as diameter decreases– Every factor of 2 change in diameter = one

step in φ

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Particle Descriptions

Name Phi Diameter mmBoulder < -8 256 +Cobble -6 to -8 64 - 256Pebble -2 to -6 4 - 64Granule -1 to -2 2 - 4Sand -2 to 4 1/16 - 2Silt 4 - 8 1/256 - 1/16Clay > 8 < 1/256

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Sediment Sizes and Clastic Rock Types

Sedimentary rocks made of silt- and clay-sized particles are collectively called mudrocks, and are the most abundant sedimentary rocks.

Rock Type Sediment Grain Size

Shale Clay less than 0.001 mm

Siltstone Silt .001-0.1 mm

Sandstone Sand .01-1 mm

Conglomerate Gravel 1mm +

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Clastic Terms

Latin Greek

Gravel Rudite Psephite

Sand Arenite Psammite

Silt Lutite Pelite

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Super-Size Me

• Blair and McPherson, J. Sed. Res., v. 69, no. 1, Jan. 1999, p. 6-19.

• Block: 4-65 m (φ = -12 to -16)• Slab: 65-1000 m (1 km) (φ = -16 to -20)• Monolith: 1-33 km (φ = -20 to -25)• Megalith: 33-1000 km (φ = -25 to -30)

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Some Special Clastic Rock Types

• Arkose Feldspar-Rich • Breccia Angular Fragments • Graywacke Angular, Immature

Sandstone

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Sandstone Terminology

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Maturity

• Stability of Minerals • Rock Fragments • Rounding or Angularity • Sorting

Removal of Unstable Ingredients - Mechanical Working

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Diagenesis

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Diagenesis

CompactionCementing• Quartz • Calcite • Iron Oxide • Clay • Glauconite • Feldspar

Alteration• Limestone - Dolomite • Plagioclase – AlbiteRecrystallization• Limestone

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Tectonic Settings and Sediment

• Cratonic: Mature sandstone• Continental slope: Graywacke, turbidite• Trench: Wildflysch (contorted graywacke)• Post-orogenic basin: Molasse (red sandstone

and conglomerate)

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Tectonic Settings and Sediment

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Lithic Sand, Washington

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Lithic Sandsone, Washington

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Molasse, Switzerland

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Molasse and the High Alps

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Conglomerates

• Clast Supported vs. Matrix Supported• Polymictic (Outwash, alluvial fans, flood

plains)• Oligomictic (Lag deposits)• Diamictic (Tills, Glacio-marine, Submarine

Landslides)

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Diamictite, Ontario