Sedimentary rocks 2
From GeoClasses
Contents |
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sedimentary basins
- weathering
- physical
- chemical
- diagenesis
- weathering exercise (requires a reading before class)
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sediment deposition
- how do you form a basin?
- subsidence
- rift basins and thermal subsidence (fig. 5.4)
- flexural basins
- Publisher's animation
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sediment transport
- currents (water)
- size, sorting, rounding
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diagenesis (how do you get a rock from sediments?)
- see fig. 5.12
- cementation, porosity, compaction
- lithification
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depositional environments
- overview with photo galleries of all subtopics can be found here
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effect of source rock on rock type:
- siliciclastic sediments
- chemical sediments
- bioclastic sediments
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sediments in the oceans
- salinity: source of salt in the ocean
- very good reading on why the ocean is salty (and rivers aren't)
- biological sediments
- evaporites
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sedimentary environments:
- see fig. 5.5
- continental:
- lake, alluvial, desert, glacial
- shoreline:
- delta, beach, tidal flat
- marine:
- deep sea, continental shelf, reefs, continental margin/slope
- carbonate platform
- see table 5.2
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sedimentary structures (and processes that form them):
- bedding and cross-bedding
- graded bedding
- ripples
- bioturbation
- bedding sequences (sequence stratigraphy)
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sedimentary rock classification
- by partical size
- by composition
- quartz arenites, arkoses, lithic sandstones, graywacke
- see fig. 5.16
- chemical and biological:
- see table 5.4
- limestone, dolomite
- coral reefs, atolls
- chert

