Sediments Flashcards

1
Q

Describe the properties of a limestone

A
  • Made of calcium carbonate
  • Non-clastic
  • Typically composed of shells of marine life etc
  • Can be chemogenic (oolitic limestones)
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2
Q

Describe sediments deposited in an aeolian environment

A
  • Fine-grained due to low density and velocity of air
  • Grains move by saltation
  • Repeated impact means grains well-rounded and high quartz content
  • Dunes, often cross-bedding
  • Common in deserts, usually red due to iron oxide (no bacteria to reduce)
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3
Q

Describe sediments deposited in a fluvial environment

A
  • Braided rivers - river struggles to transport sediment (a lot or coarse - upstream)
  • Transport during seasonal high water levels
  • Movement as bedload
  • Coarse grained
  • Meandering river - flow more efficient
  • Transport as suspended and bedload
  • Alternating layers of mudrock and sandstone due to floods (heterolithic sediment)
  • Calcretes: carbonate precipitates from ground water around roots, forming thick CaCO3 layers in mudrock
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4
Q

Describe sediments deposited in a deltaic environment

A
  • Coarsening upwards - delta progrades (moves out to sea)
  • Sediments sorted by distance travelled suspended in sea
  • Hence as delta moves out coarser sediments overlay finer ones
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5
Q

Describe sediments deposited in a glacial environment

A
  • Can be very large (>10m) - ice is low velocity and high viscosity
  • Till - glacial sediment deposit when melts
  • Poorly sorted matrix supported conglomerate (diamictite)
  • Icebergs with large rocks float to sea - dropstones
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6
Q

What is a clastic sediment?

A

Composed of grains separated from a parent rock by erosion

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7
Q

What is a carbonate sediment?

A

Typically non-clastic, formed of CaCO3 grains, either from skeletons of organisms or precipitated from ocean (ooids)

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8
Q

What is a sedimentary log?

A

Graphical representation of vertical rock sections. x axis is grain size, y axis is time.

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9
Q

What is a regolith?

A

A rock loosened by erosion, available for transport by fluids

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10
Q

Describe sediments deposited in a turbidite environment

A
  • Turbidite (water plus sediment) moves down shelf under gravity
  • Deposits sediments in order (Bouma sequence) - graded bedding
  • Fining up with time
  • Submarine fan: sediment originates from point source (eg underwater canyon). Turbidites flow for long distances
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11
Q

Describe the physics of entrainment

A
  • Entrainment - when the force is just great enough to move a sediment
  • Lift force provided by Bernoulli effect
  • Greater velocity required for less dense fluid (air)
  • Drag and push force from fluid
  • Suspended load maintained by buoyancy (Archimedes)
  • Laminar flow better at entrainment (low Reynolds number)
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12
Q

Draw and explain the Hjulstrom diagram

A
  • Shows relationship between critical flow velocity (v required to transport sediment) and grain size
  • In general, larger grains = greater velocity needed
  • Hence larger grains settle first as v decreases, this leads to sorting
  • Erosion leads to roundedness
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13
Q

Describe erosive processes creating a regolith

A
  • Chemical weathering - solution, hydrolysis, oxidation
  • Physical weathering - salt growth, freeze-thaw, biological intrusion (roots)
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14
Q

Explain what leads to graded bedding

A
  • Graded bedding - within a bed, grains become coarser/finer along an axis
  • Due to changes in flow velocity leading to different-sized grains settling
  • Decreasing velocity - fines upwards
  • Increasing velocity - coarsens upwards
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15
Q

Which minerals are more resistant to weathering, so more likely to be found in sedimentary rocks?

A
  • Felsic minerals more resistant - sedimentary rocks have high quartz content, some feldspars
  • Clay minerals formed during erosion or diagenesis
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16
Q

What is clay?

A
  • Clay is an ultrafine-grained, cohesive sediment made of clay minerals
  • Formed during erosion of parent rock or diagenesis of sedimentary rock
  • Sheet silicates with Si and Al tetrahedra
  • eg chlorite, kaolinite
17
Q

What is the Uden-Wentworth scale?

A
  • Classifies rocks by grain size
  • Based on logarithmic phi scale
  • phi = -log2(grain size)
18
Q

Describe the flow regime leading to ripples and cross-lamination

A
  • Low velocity flow regime
  • Erratic eddy currents cause grains to cluster
  • Moving fluid pushes sediment up the slope (stoss side)
  • Sediment crests and flow separates, causing avalanches down lee slide, accumulation
    *Cluster grows into a ripple
  • New ‘slopes’ preserved as downstream-dipping laminae (cross-lamination - at an angle to bedding)
  • Either planar or concave-upwards (trough)
19
Q

Describe the flow regime leading to dunes and cross-bedding

A
  • Low velocity flow regime
  • Stronger flow than ripples
  • Ripples reworked into dunes (different features - discontinuity)
  • Dunes have larger wavelength and height
  • Eddy currents push sediment up the steep face of the dune (reverse flow)
  • Dunes create cross-bedding
20
Q

Describe the flow regime leading to plane bedding and planar lamination

A
  • Could be zero flow (lower plane bed)
  • Could also be intermediate flow regime
  • Stronger flow washes out dunes (entrainment)
  • Increased sediment (bedload and suspended) dampens the effect of turbulence
  • Forms a flat upper plane bed with planar lamination
21
Q

Describe the flow regime leading to antidunes

A
  • High flow regime
  • Rare in sedimentary record
  • Flow so high that fluid moves faster than waves on its surface
  • Hence waves move upstream, steepen and then break (collapse on themselves)
  • Moves sediment to form antidunes with laminae dipping upstream
22
Q

Describe bedforms created in bidirectional flow regimes

A
  • Symmetrical
  • Formed if water depth less tha wavebase
23
Q

What determines if an environment is depositional or erosional?

A

Evidence of erosional environment:
* Dessication cracks
* Raindrop impressions

24
Q

What are the types of sedimentary basin?

A
25
Q

Describe sediments deposited in lacustrine environments

A
  • Organic rich sediments (anoxic seafloor)
  • Clastic sediment from feeder river (fluvial)
  • Evaporites (gypsum, halite) when lake dries up
26
Q

Describe sediments deposited in alluvial fan environments

A
  • Water exits mountain valleys and fans out
  • Common at margins of basins
  • Debris flows - water/sed mix flows short distance under gravity
  • Coarse grained
  • Poorly sorted matrix supported conglomerate
  • Imbrication: pebbles dip upstream
27
Q

Describe sediment deposited in coastal environments

A
  • Sediment supplied by rivers, moved by longshore drift
  • Carbonate coasts: ooids/biogenic material deposited
  • Arid climate: hypersaline lagoons. Evaporites gypsum and anhydrite.
28
Q

Describe sediment deposited in marine carbonate environments

A
  • Shallow marine - seds have biological origin
  • Complete skeletal remains or bioclasts (fragments)
  • Stromatolites - calcified microbial mats
  • Ooids - carbonate precipitated around a nucleus (usually a bioclast)
29
Q

Describe sediments deposited in shallow marine environments

A
  • Dominated by tide and wave processes
  • Herringbone crossbedding - dip in opposite directions due to bidirectional tide
  • Storm waves generate Hummocky cross-stratification (mounds)