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
Q

U shaped burrows inidcate…

A

rapid sedimenation

26
Q

What can these be used to do (with regards to superposition)

A

They can be used to work out if there bed has been turned upside down (anticline)