Introduction and stratigraphic methods Flashcards

1
Q

What can stratigraphy be used for?

A

Determining tectonic, biological, and climatic events

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2
Q

What are the two ways to determine geological age?

A

Relatively or numerically

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3
Q

Define relative geological aging

A

Placing rocks and events in their proper sequence of formation/occurence
Lithostratigraphy

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4
Q

Define numerical (absolute) geological aging

A

Specifying absolute number of years since an event
Geochronology

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5
Q

Describe the principle of superposition

A

Relative aging
Each bed is younger than the one below it
Thrust faulting can invert the order

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6
Q

Describe the principle of cross-cutting

A

Relative aging
A bed or unit is younger than the one it cuts across

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7
Q

Describe the principle of original horizontality

A

Relative aging
Consolidated strata that are now tilted were originally deposited horizontally

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8
Q

Describe the principle of continuity

A

Relative aging
In a basin, the same bed is of identical age in every part, beds terminate were deposition was not possible or where they have been eroded or deformed after deposition

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9
Q

Describe the principle of inclusion

A

Relative aging
If an element A is included in an element B, A is older than B

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10
Q

Describe palaeontological identity

A

Relative aging
All beds including the same fossils are of the same age
Relies of the principle of faunal succession
Not applicable where there has been reworking

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11
Q

Describe an unconformity

A

Relative aging
A break in the geological record produced by erosion and/or non-deposition

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12
Q

Describe an angular unconformity

A

Relative aging
Tilted rocks are overlain by flat-lying rocks

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13
Q

Describe a disconformity

A

Relative aging
Strata on either side a parallel, there have been a period of erosion

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14
Q

Describe a non-conformity

A

Relative aging
Metamorphic or ignous rocks in contact with sedimentary strata

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15
Q

Describe isotopic ratios

A

Relative aging
Applicable when changes are globally synchronous
O2 linked to temp
C linked to biological activity
S linked to igneous processes
Correlates within basin
Supported by absolute age dates

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16
Q

Define uniformitarianism

A

The same processes operating today were active in the past

17
Q

Define numerical (absolute) geological aging

A

Specifying the absolute number of years since an event

18
Q

Describe radioactive decay

A

Absolute aging
Time that it takes U to decay to Pb (parent to daughter isotope)

19
Q

What does the use of radioactive decay for absolute dating require?

A

A closed system that contains no original daughter nuclides

20
Q

Describe mangetostratigraphy

A

Absolute aging
Magnetic minerals orient to the pole
Pole changed from S to N ~700,000 ya
Minerals formed before this will orient to old pole

21
Q

When do magnetic minerals orient to the pole?

A

Below the Curie point, ~570C, above this they orientate in random directions

22
Q

Describe radiocarbon (C-14) dating

A

Absolute aging of organic material
Upper limit of ~70,000 years

23
Q

Define chronostratigraphic units

A

The relative relations and ages of rock bodies

24
Q

Define geochronological units

A

Dating and determining the time sequnce of depositional/deformity events
Provides absolute ages

25
Q

Give an example of how a bed can be destroyed

A

By compaction during lithification
This compaction can make it so the bed’s thickness no longer indicates geological time

26
Q

What is the subdivision of stratigraphic units based on?

A

Their lithological character and stratigraphy
Boundaries are placed at lithological changes (can be sharp/gradational)

27
Q

Give the subdivision of stratigraphic units, in order from smallest to largest

A

Bed, member, formation, group, supergroup

28
Q

Describe a bed subdivision

A

Smallest unit, can be a key/marker bed, a thin distinctive bed that is widely distributed

29
Q

Describe a member subdivision

A

Part of formation with distinguishing traits

30
Q

Describe a formation subdivision

A

Fundamental unit

31
Q

Describe a group subdivision

A

Expresses natural relations beween formations
Small to regional scale

32
Q

Describe supergroup subdivsion

A

Assemblage of related or superposed groups
Regional to provincial scale

33
Q

What does biostratigraphy depend on?

A

Species evolve into new forms and have a discreet duration before becoming extinct

34
Q

What defines a biozone?

A

The assemblage of index fossils

35
Q

What is a limitation of biostratigraphy?

A

The biases of the rock record and taphonomy
Organisms can evolve at different rates around the world

36
Q

Describe radiometric dating

A

Absolute aging
Radioactive clock measures time of crystallisation

37
Q

Give four requirement of geochronology that can limit its efficacy

A

Requires a closed system with no original daughter nuclides (Pb), fresh samples, and a variety of minerals

38
Q
A