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Detrital Sedimentary Rocks |
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Nonorganic, solid particles put through both mechanical and chemical weathering. Clay minerals and quartz are the chief constituents of most detrital rocks. 85% of all sedimentary rocks. chemical resistant. Composed of minerals with slow rates of chemical weathering, or the products of chemical weathering. Composition varies with weathering intensity or length of transport.
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Chemical Sedimentary Rocks |
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When ions in solution are precipitated by either inorganic or biological processes, the material is known as chemical sediment, and it makes these rocks. |
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Organic Sedimentary Rocks |
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Coal is a prime example; when carbonic plant matter is cemented left over from swamps. |
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variety of minerals and rock fragments. |
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Store solar energy and provide a look into the past. |
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Depositional Environments |
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from Glaciers, rivers, dunes are created from wind, shores, both from ocean and river |
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making sedimentary rocks through compaction and cementation |
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Common cementation elements |
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- silica (SiO3)
- calcium carbonate (CaCO3)
- iron oxide (Fe2O3-H2O)
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Compaction relative to clay |
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Clays may be compact up to 40% |
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all low-temperature chemical changes that happen under the surface |
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- Quartz sandstone-mostly quartz
- arkose sandstone- angular grains, feldspars and rock fragments
- graywacke-dirty sandstone, has quartz, feldspar, clays
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Difference between breccia and conglomerate? |
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Definition
conglomerate uses rounded grain, breccia-angular |
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Siltstone, mudstone, shale |
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- Siltstone-mostly silt
- Mudstone- silt and clay, not shale-like layers
- Shale- red means oxygen present
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Precipitation sequence from seawater: |
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Definition
1) Calcite (CaCO3) 2) Gypsum (CaSO4·2H2O) 3) Halite (NaCl) |
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Chemical Sedimentary Rocks |
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Biochemical sedimentary rocks = biogenic precipitates » biogenic = originates from life
Limestone - mostly calcite; often composed of biogenic grains which may recrystallize » Typically deposited where there is little or no clastic sediment » Can vary from of fossil-free to fossiliferous |
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Cementation differences between chemical rocks |
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coquina-badly cemented, chalk is good |
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–Formed by trapping of sediment by algae *Evidence for shallow water –Some of the earliest fossils |
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- biogenic buildup; carbonate secreting organisms; marine –Evidence for shallow water |
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SiO2, micro- or cryptocrystalline »Remains of silica-secreting microorganisms living in ocean (diatoms, radiolaria) »Also forms from silica precipitation in pores after burial |
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asymmetrical-waves go 1 way
oscillatory-goes both ways |
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grain size decreases upward »Caused by slowing of current |
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burrows, footprints, root traces |
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major parts of shields and mountain belts |
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Process whereby preexisting rock undergoes pronounced changes in texture and mineralogy at T > 200-300ºC while in the solid state |
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heat, pressure, chemically active fluids, heat gets greater as you go down |
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Increased ductility – Change in mineral assemblage |
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Confining pressure - felt equally in all directions » Differential stress - added pressure from tectonic activity (tension, compression, shear) |
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Favors minerals with dense, compact crystal structures » Minerals grow perpendicular to maximum pressure – Produces a parallel arrangement of platy minerals called foliation – Gives rock layered or banded appearance |
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shallow crustal rocks are metamorphosed by increasing T. |
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sediments are metamorphosed by increasing P and T |
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sedimentary strata are meta-morphosed by moderately increasing P and T |
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Hydrothermal fluids (hot water); important for ion transport |
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»Rock or slaty cleavage - parallel alignment of microscopic platy minerals »Schistosity - parallel alignment of visible platy minerals |
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banded; layers of light and dark minerals |
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Lineation - parallel alignment of needle-like grains Porphyroblastic - larger crystals (porphyroblasts) in a finer matrix |
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Supplies ions/atoms; can alter composition inherited from protolith |
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very fine grained, clay rich »Slaty cleavage »Bedding often present »Metamorphic grade: low |
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Cleavage surface has sheen »Mica and/or chlorite grains Figure 8.14 AN07_004. |
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50% visible platy minerals; may have layers or qtz and/or feldspar »Bedding rare »Grade: medium to high »Rock name based on predominant mineral –Ex: muscovite schist (clay |
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Fine to coarsely crystalline calcite »Parent: limestone or dolomite |
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Metamorphosed qtz sandstone; almost all qtz |
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Metamorphosed conglomerate - breaks through pebbles |
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»Contains glaucophane (amphibole) »High pressure, relatively low temperature |
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pyx, garnet; high P, moderate T |
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three types of metamorphism |
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»Contact - associated with plutonism; small scale »Cataclastic - occurs within fault; very small scale »Regional - associated with mountain-building; large scale |
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zone of metamorphosed rock around pluton; non-foliated |
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unique rock formed from metamorphism of protolith of silicate and carbonate (limestone or dolomite) rocks |
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broken and crushed rock in fault |
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hard, fine-grained rock formed from grinding within fault |
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