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Sedimentary rocks

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ROCK CYCLE

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Relative Percentages of
Sedimentary Rocks

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SEDIMENT
 From
 Weathering & Erosion
 Precipitation from saturated solution
 calcite, quartz
 Product of evaporation
 halite, gypsum
 Unconsolidated- NOT cemented

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SEDIMENT
 Particle size
 Pebbles, cobbles, boulders
 Gravel- > 2mm
 Sand- 2mm - 0.063mm
 Silt - 0.063mm - 0.004mm
 Clay- < 0.004
 Deposition Clay-sized particle vs. clay mineral

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SEDIMENT
 Transportation
 Abrasion
 Rounding
 Sorting
 Deposition
 Environment of deposition- specific
 Preservation

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENT
 Transportation
 Abrasion
 Rounding
 Sorting
 Deposition
 Environment of deposition- specific
 Preservation

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENT
 Lithification
 Compaction
 Decrease in pore space
 for very fine grain size (clay)
 Cementation
 Clastic texture
 Cements- silica, calcite, iron oxide
 Crystallization
 Crystalline texture

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENT
 Lithification
 Compaction
 Decrease in pore space
 for very fine grain size (clay)
 Cementation
 Clastic texture
 Cements- silica, calcite, iron oxide
 Crystallization
 Crystalline texture

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENT
 Lithification
 Compaction
 Decrease in pore space
 for very fine grain size (clay)
 Cementation
 Clastic texture
 Cements- silica, calcite, iron oxide
 Crystallization
 Crystalline texture

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23.3.d sedimentary rocks ppt.ppt

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TYPES OF SEDIMENTARY
ROCKS
 Clastic or Detrital
 Chemical- inorganic precipitation or
evaporation
 Biochemical- Organic remains
 shells, charcoal, plant fragments

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CLASTIC (Detrital) ROCKS
 Breccia and Conglomerate (> 2mm)
 Sedimentary Breccia- angular fragments
 Conglomerate- rounded fragments
 Sandstone (2mm - 0.063mm)
 Quartz sandstone
 Arkose (feldspar)
 Graywacke (appreciable amounts of silt/clay)
 Fine-grained Matrix
 Usually from turbidity currents

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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CLASTIC (Detrital) ROCKS
 Breccia and Conglomerate (> 2mm)
 Sedimentary Breccia- angular fragments
 Conglomerate- rounded fragments
 Sandstone (2mm - 0.063mm)
 Quartz sandstone
 Arkose (feldspar)
 Graywacke (appreciable amounts of silt/clay)
 Fine-grained Matrix
 Usually from turbidity currents

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Quartz Sandstone

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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CLASTIC ROCKS
 Fine-grained Rocks
 Shale- fissile (in ‘sheets’)
 Siltstone
 Claystone
 Mudstone (silt and clay)

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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CHEMICAL SEDIMENTARY
ROCKS
 Carbonate Rocks
 Limestone- made of calcite
 Inorganic varieties
 micrite, oolites, travertine
 Dolomite
 Recrystallization
 Chert- silica
 Evaporites
 Rock gypsum
 Rock salt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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BIOCHEMICAL
SEDIMENTARY ROCKS
 Coal
 Develops from peat
 plant fragments
 Lignite
 Bituminous Coal
 Carbonate Rocks
 Limestone- made of calcite
 organic varieties
 Coquina
 Fossiliferous Limestone
 Chalk

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23.3.d sedimentary rocks ppt.ppt

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BIOCHEMICAL
SEDIMENTARY ROCKS
 Coal
 Develops from peat
 plant fragments
 Lignite
 Bituminous Coal
 Carbonate Rocks
 Limestone- made of calcite
 organic varieties
 Coquina
 Fossiliferous Limestone
 Chalk

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENTARY
STRUCTURES
 BEDDING-
 Principle of Original Horizontality
 Bedding plane
 Cross-bedding
 Graded bed
 Mud cracks
 Ripple marks
 Fossils

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENTARY
STRUCTURES
 BEDDING-
 Principle of Original Horizontality
 Bedding plane
 Cross-bedding
 Graded bed
 Mud cracks
 Ripple marks
 Fossils

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DUNES

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENTARY
STRUCTURES
 BEDDING-
 Principle of Original Horizontality
 Bedding plane
 Cross-bedding
 Graded bed
 Mud cracks
 Ripple marks
 Fossils

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENTARY
STRUCTURES
 BEDDING-
 Principle of Original Horizontality
 Bedding plane
 Cross-bedding
 Graded bed
 Mud cracks
 Ripple marks
 Fossils

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Mudcracks

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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SEDIMENTARY
STRUCTURES
 BEDDING-
 Principle of Original Horizontality
 Bedding plane
 Cross-bedding
 Graded bed
 Mud cracks
 Ripple marks
 Fossils
 Body Fossils
 Trace Fossils

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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INTERPRETATION OF
SEDIMENTARY ROCKS
 Source Area
 Environment of Deposition
 Glacial environments
 Tillites
 Alluvial fan
 Arkose
 River channel and flood plain
 Interbedded shales and sandstones; cross-bedded
 Lake
 Shales; interbedded siltstones and mudstones
 Delta

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23.3.d sedimentary rocks ppt.ppt

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Glacial Environment & Till

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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INTERPRETATION OF
SEDIMENTARY ROCK
 Environment of Deposition
 Beach, Barrier Island, Dune
 Very well sorted quartz sandstones
 Lagoon
 Shales
 Shallow marine shelf
 Interbedded sandstones and shales; burrowed
 Reef
 Skeletal Limestones
 Deep marine environment
 Turbidites- sequence of GRADED sandstones to shales

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23.3.d sedimentary rocks ppt.ppt

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INTERPRETATION OF
SEDIMENTARY ROCK
 Environment of Deposition
 Beach, Barrier Island, Dune
 Very well sorted quartz sandstones
 Lagoon
 fine grained sediment
 Shallow marine shelf
 Interbedded sandstones and shales; burrowed
 Reef
 Skeletal Limestones
 Deep marine environment
 Turbidites- sequence of GRADED sandstones to shales

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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CALCAREOUS

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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INTERPRETATION OF
SEDIMENTARY ROCK
 Environment of Deposition
 Beach, Barrier Island, Dune
 Very well sorted quartz sandstones
 Lagoon
 Shales
 Shallow marine shelf
 Interbedded sandstones and shales; burrowed
 Reef
 Skeletal Limestones
 Deep marine environment
 Turbidites- sequence of GRADED sandstones to shales

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23.3.d sedimentary rocks ppt.ppt

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23.3.d sedimentary rocks ppt.ppt

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INTERPRETATION OF
SEDIMENTARY ROCK
 Plate Tectonics and Sedimentary Rocks
 At convergent boundaries
 Uplift results in
 Very rapid rates of erosion
 Thick accumulations of clastic sediment
 At transform boundaries
 Rapid rates of erosion, deposition and burial
 Good basins for petroleum exploration
 At divergent boundaries
 Initial stages of rifting- thick wedges of gravel and
coarse sediment

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Resources
 Non-Metallic
 Sand and gravel
 Limestone
 Clay
 Gypsum
 Energy Resources
 Oil and gas
 Coal

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Formation of Oil and Gas

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Thank you…

More Related Content

23.3.d sedimentary rocks ppt.ppt

  • 4. SEDIMENT  From  Weathering & Erosion  Precipitation from saturated solution  calcite, quartz  Product of evaporation  halite, gypsum  Unconsolidated- NOT cemented
  • 5. SEDIMENT  Particle size  Pebbles, cobbles, boulders  Gravel- > 2mm  Sand- 2mm - 0.063mm  Silt - 0.063mm - 0.004mm  Clay- < 0.004  Deposition Clay-sized particle vs. clay mineral
  • 6. SEDIMENT  Transportation  Abrasion  Rounding  Sorting  Deposition  Environment of deposition- specific  Preservation
  • 10. SEDIMENT  Transportation  Abrasion  Rounding  Sorting  Deposition  Environment of deposition- specific  Preservation
  • 13. SEDIMENT  Lithification  Compaction  Decrease in pore space  for very fine grain size (clay)  Cementation  Clastic texture  Cements- silica, calcite, iron oxide  Crystallization  Crystalline texture
  • 15. SEDIMENT  Lithification  Compaction  Decrease in pore space  for very fine grain size (clay)  Cementation  Clastic texture  Cements- silica, calcite, iron oxide  Crystallization  Crystalline texture
  • 17. SEDIMENT  Lithification  Compaction  Decrease in pore space  for very fine grain size (clay)  Cementation  Clastic texture  Cements- silica, calcite, iron oxide  Crystallization  Crystalline texture
  • 19. TYPES OF SEDIMENTARY ROCKS  Clastic or Detrital  Chemical- inorganic precipitation or evaporation  Biochemical- Organic remains  shells, charcoal, plant fragments
  • 20. CLASTIC (Detrital) ROCKS  Breccia and Conglomerate (> 2mm)  Sedimentary Breccia- angular fragments  Conglomerate- rounded fragments  Sandstone (2mm - 0.063mm)  Quartz sandstone  Arkose (feldspar)  Graywacke (appreciable amounts of silt/clay)  Fine-grained Matrix  Usually from turbidity currents
  • 23. CLASTIC (Detrital) ROCKS  Breccia and Conglomerate (> 2mm)  Sedimentary Breccia- angular fragments  Conglomerate- rounded fragments  Sandstone (2mm - 0.063mm)  Quartz sandstone  Arkose (feldspar)  Graywacke (appreciable amounts of silt/clay)  Fine-grained Matrix  Usually from turbidity currents
  • 28. CLASTIC ROCKS  Fine-grained Rocks  Shale- fissile (in ‘sheets’)  Siltstone  Claystone  Mudstone (silt and clay)
  • 31. CHEMICAL SEDIMENTARY ROCKS  Carbonate Rocks  Limestone- made of calcite  Inorganic varieties  micrite, oolites, travertine  Dolomite  Recrystallization  Chert- silica  Evaporites  Rock gypsum  Rock salt
  • 34. BIOCHEMICAL SEDIMENTARY ROCKS  Coal  Develops from peat  plant fragments  Lignite  Bituminous Coal  Carbonate Rocks  Limestone- made of calcite  organic varieties  Coquina  Fossiliferous Limestone  Chalk
  • 36. BIOCHEMICAL SEDIMENTARY ROCKS  Coal  Develops from peat  plant fragments  Lignite  Bituminous Coal  Carbonate Rocks  Limestone- made of calcite  organic varieties  Coquina  Fossiliferous Limestone  Chalk
  • 40. SEDIMENTARY STRUCTURES  BEDDING-  Principle of Original Horizontality  Bedding plane  Cross-bedding  Graded bed  Mud cracks  Ripple marks  Fossils
  • 43. SEDIMENTARY STRUCTURES  BEDDING-  Principle of Original Horizontality  Bedding plane  Cross-bedding  Graded bed  Mud cracks  Ripple marks  Fossils
  • 44. DUNES
  • 47. SEDIMENTARY STRUCTURES  BEDDING-  Principle of Original Horizontality  Bedding plane  Cross-bedding  Graded bed  Mud cracks  Ripple marks  Fossils
  • 50. SEDIMENTARY STRUCTURES  BEDDING-  Principle of Original Horizontality  Bedding plane  Cross-bedding  Graded bed  Mud cracks  Ripple marks  Fossils
  • 55. SEDIMENTARY STRUCTURES  BEDDING-  Principle of Original Horizontality  Bedding plane  Cross-bedding  Graded bed  Mud cracks  Ripple marks  Fossils  Body Fossils  Trace Fossils
  • 61. INTERPRETATION OF SEDIMENTARY ROCKS  Source Area  Environment of Deposition  Glacial environments  Tillites  Alluvial fan  Arkose  River channel and flood plain  Interbedded shales and sandstones; cross-bedded  Lake  Shales; interbedded siltstones and mudstones  Delta
  • 66. INTERPRETATION OF SEDIMENTARY ROCK  Environment of Deposition  Beach, Barrier Island, Dune  Very well sorted quartz sandstones  Lagoon  Shales  Shallow marine shelf  Interbedded sandstones and shales; burrowed  Reef  Skeletal Limestones  Deep marine environment  Turbidites- sequence of GRADED sandstones to shales
  • 68. INTERPRETATION OF SEDIMENTARY ROCK  Environment of Deposition  Beach, Barrier Island, Dune  Very well sorted quartz sandstones  Lagoon  fine grained sediment  Shallow marine shelf  Interbedded sandstones and shales; burrowed  Reef  Skeletal Limestones  Deep marine environment  Turbidites- sequence of GRADED sandstones to shales
  • 74. INTERPRETATION OF SEDIMENTARY ROCK  Environment of Deposition  Beach, Barrier Island, Dune  Very well sorted quartz sandstones  Lagoon  Shales  Shallow marine shelf  Interbedded sandstones and shales; burrowed  Reef  Skeletal Limestones  Deep marine environment  Turbidites- sequence of GRADED sandstones to shales
  • 77. INTERPRETATION OF SEDIMENTARY ROCK  Plate Tectonics and Sedimentary Rocks  At convergent boundaries  Uplift results in  Very rapid rates of erosion  Thick accumulations of clastic sediment  At transform boundaries  Rapid rates of erosion, deposition and burial  Good basins for petroleum exploration  At divergent boundaries  Initial stages of rifting- thick wedges of gravel and coarse sediment
  • 78. Resources  Non-Metallic  Sand and gravel  Limestone  Clay  Gypsum  Energy Resources  Oil and gas  Coal
  • 79. Formation of Oil and Gas