Lecture 4 - Sedimentary Structures Flashcards

1
Q

Define bedding:

A

Sedimentary layer thicker than 1cm (can be done in hours or 100s of years)

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2
Q

Define lamination:

A

Fine scale bedding, less that 1 cm thick

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3
Q

What effects the type of bedforms made?

A

Verlocity of the flow, grain size, depth of flow.

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4
Q

What can happen to these bedrocks to help us learn about the past

A

these structures can become fossilised

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5
Q

What does the absense of lamination show?

A

Bioturbidation

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6
Q

Can you draw a diagram about the formation of ripples?

A

Yes

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7
Q

What are the different bedform types?

A

Ripples
Sandwaves
Dunes

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8
Q

What gorms waves as aposses to ripples

A

Waves are formed by two currents meaning deposition and eroisin is equal on either side

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9
Q

Ripples. Slowest to fastest

A

straight crested
sinuous
catenary

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10
Q

Dunes slowest to fastst

A

lunate

lingouid

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11
Q

what are the differencens between two dimesnial and three dimesnal crests

A

straight crested ripples are the only 2D ones as they are just parrel lines

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12
Q

What is the Herring bone cross bedding associated with?

A

Tidal regieme, two undirectional currents at 180 degrees to each other. although it can be difficult to distingues between these waves and ripples.

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13
Q

In general what sets waves apart

A

Sharper crests, more symetrical cross section.

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14
Q

The above are straight unidrection currents what are the others more complex currents known as

A

Turbidity currents

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15
Q

What are turbidity currents

A

Sediment laden (turbid), fast flowing, common on seafloor. sediment often disturbed by storms or earth quakes.

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16
Q

Can you draw a flute mark? also explain a flute mark

A

Sand laded current erodes and marks cohesivce mud prior to deposition creating a half conical shape in the mud. These are then in filled with depoistion creating smooth conical flute marks.

17
Q

What are groove marks?

A

Objects carried in flow groove into the mud, the space is filled in by the turbidite sediment

18
Q

Wjat is graded bedding?

A

Graded bedding is where the larger rocks settle out first and then as it goes up the smaller sediments settle.

19
Q

What is the sequence of these graded beds called

A

Bouma Sequence

20
Q

What do mudcracks show?

A

Subarial exposure, in a dry climate causing the rocks to dry out.

21
Q

What are trace fossils?

A

These are “traces” or marks in the sediment that are made by an activity, they are not classfied by organisms

22
Q

What are the two mains groups of trace fossils?

A

1) formed on sediment surface such as tracks and trails EPIBENTHIC
2) formed within a sediment such as burrows ENDOBENTHIC

23
Q

Sedimentation rates, what do borings or burrows show

A

There is zero sedimenation

24
Q

Intenstly bioturbated sediment indicates

A

slow sedimentation

25
U shaped burrows inidcate...
rapid sedimenation
26
What can these be used to do (with regards to superposition)
They can be used to work out if there bed has been turned upside down (anticline)