Lecture 2 Flashcards

1
Q

Who first observed unconformity and when

A

Hutton and playfair in 1788

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2
Q

Siccar point unconformity

A

a surface with horizontal Devonian sandstones on top of almost vertical silurian slates

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3
Q

Geological cycle

A
  • Sedimentation
  • Burial
  • Folding, faulting, mountain-forming and igneous intrusion
  • Erosion
    Back to sedimentation as eroded rocks transported by rivers
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4
Q

What is lithophagia

A

when organisms gain nutrients from rocks—>form of erosion

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5
Q

What did Ussher work on

A

He was an archbishop and in 1654 estimated the creation of the earth at 4004 BC based on the bible

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6
Q

Lord kelvin’s contribution

A

Using loss of heat from a sphere he estimated 40-100 million years old—>however made many invalid assumptions

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7
Q

Stratigraphy

A

The study of rock layers in order to determine relative ages and therefore form a relative geological timescale

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8
Q

4 laws of stratigraphy

A
  1. Superposition, so rocks on top are newer
  2. Lateral continuity, so if rocks eroded away then lateral construction can be formed as originally continuous
  3. Initial horizontality, assumption that strata were formed relatively horizontally
  4. Cross-cutting relations
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9
Q

Biostratigraphy

A

Stratigraphy with fossils and fossil zones as these are generally more uniform than the differing conditions across the surface of earth which leads to different rock types

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10
Q

Facies

‘fash-ees’

A

environment of deposition. SO different environments can exist in different places at the same time, so mud and sand on river estuary and beach.

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11
Q

Problems with biostratigraphy

x5

A
  1. facies
  2. Many rocks lack fossils, especially continental ones
  3. Fossil zones may not extend beyond a single continent, if that far
  4. Few useful fossils prior to Cambrian and evolution of hard parts and almost 90% history before that
  5. Gaps are common—>called an unconformity
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12
Q

Unit Ma

A

Means million years before present

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13
Q

What is chalk formed of

A

Mainly coccolithophores, which are formed of CaCO3

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14
Q

Break between proterozoic and cambrian

A

Evolution of ‘hard’ parts, bone, shells and other less fleshy parts

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15
Q

Paleozoic to Mesozoic

A

Volcanic eruption in siberia

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16
Q

Mesozoic to Cenozoic

A

Asteroid impact removed charismatic megafauna

17
Q

Pliocene to Pleistocene

A

Development of ice sheets in the northern hemisphere

18
Q

The decay of parent, P, isotopes to stable daughter, D, isotopes gives us a clock, what equations do we use.

A

GRAPH 5

19
Q

What are the most common systems used in radioactive dating

A

Rb—>Sr
Thorium and uranium to lead
Potassium to argon
Carbon to nitrogen

20
Q

Best crystal to test

A

Zircons in Jack Hills
4.4B
No lead when formed but some uranium so any lead present was due to decay

21
Q

Only closed systems are dated. Why?

A

IF the daughter atoms are lost we need to reset the clock as it makes it look younger than it is.
Closure occurs when below closure temp which changes due to isotope system and mineral involved.

22
Q

Why is zircon a good closed system

A

Closes at >750 degrees so very close to actual formation time

23
Q

What do we actually mean by date?

—why do we have to ask that question?

A

Age of deposition of the sediment may be much younger than the formation of the crystals within it

24
Q

Estimate of the earths age using U-Pb system

A

~4560Ma

25
Q

How good is stratigraphic correlation?
Using the example between deep-sea boreholes in the Southern Ocean
-GRAPH

A
  1. Magnetic polarity, rock types and fossil zone shown
  2. Rock type does not correlate at all (variability of facies)
  3. Magnetic polarity reversals are effectively synchronous everywhere
  4. Sedimentation rates very variable
  5. Fossil zone correlate quite well with the magnetic reversals