The document discusses sedimentary rocks, describing their formation from weathering and erosion of pre-existing rocks. Sediment is transported via water or wind and sorted by size into gravel, sand, silt, or clay. Sediment is then deposited and may undergo lithification into sedimentary rock through compaction and cementation. The main types of sedimentary rocks are clastic (formed from fragments), chemical (formed from precipitation), and biochemical (containing organic material). Sedimentary structures provide clues about the environment of deposition, and the interpretation of these rocks can reveal information about past plate tectonic settings and conditions. Sedimentary rocks are an important source of non-metallic and energy resources.
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