1. Introduction Flashcards

1
Q

What are the two types of geological age?

A

Relative geological ages: placing rocks and events in their proper relative sequence of formation/occurence
Absolute geological ages: specifying absolute number of years since an event

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2
Q

What are the stratigraphic principles of relative dating?

A

superposition: each bed is younger than the one below it
cross cutting: a bed (or unit) is younger than the one it cuts through
original horizontality: consolidated strata that are tilted now were originally deposited horizontal
continuity: in a basin, the same bed is of identical age in every part of the basin
inclusion: if an element A is included in an element B, then A is older than B
paleontological identity: all beds including the same fossils are of the same age, unless reworked

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3
Q

Define unconformity

A

break in the rock record produced by erosion and/or non deposition

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4
Q

Define uniformitarianism

A

Same processes operating today were active in the past: “the present is the key to the past”

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5
Q

Define angular unconformity

A

tilted rocks are overlain by flat-lying rocks

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6
Q

define disconformity

A

strata on either sides are parallel

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7
Q

define nonconformity

A

metamorphic or igneous rocks in contact with sedimentary strata

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8
Q

what is faunal succession?

A

observation that assemblages of fossil plants and animals follow or succeed each other in time in a predictable manner, even when found in different places

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9
Q

How are absolute geological ages defined?

A

Using Marie Curies research into the halflives of radioactive isotopes

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10
Q

What effects our concept of geological time? How can we combat these?

A
  • Gaps in the rock record
  • rates of deposition

A chronostratigraphic diagram, using units of time in the y axis, can be shown alongside the stratigraphic log that uses thickness on the y axis

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11
Q

What are the techniques used to relatively date rocks
- what material do you need

A

1) Lithostratigraphy
- Lithology
2) Biostratigraphy
- Fossils
3) Isotope stratigraphy
- Geochemical data

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12
Q

What are the techniques used to absolutely date rocks
- what material do you need

A

1) Radiocarbon ( C-14)
- Organic material
2) Uranium-lead and others
- various U,K minerals
3) Magnetostratigraphic
- Volcanic and sedimentary rocks

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13
Q

What is lithostratigraphy?

A

Subdivision of stratigraphic units on the basis of their lithological character and stratigraphic position

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14
Q

What is the lithostratigraphic hierarchy

A

1) Supergroup: Assemblage of related groups (regional to provincial scale)
2) Group: relations between formations (small to regional scale)
3) Formation: Fundamental unit
4) Member: Part of formation with distinguishing traits
5) Bed: smallest unit
6) Key or marker bed: thin distinct bed that is widely distributed

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15
Q

how does bio stratigraphy date rocks?

A

Species evolve into new forms and have a discreet duration before becoming extinct, biozone boundaries characterised by index fossils
- they need to be widespread, can’t be restrictive to certain environments, has a specific morphology.

Need to be combined with absolute ages (of surrounding beds and fossils contained) to be useful and not only give relative ages

periods of geological time may be characterized by:
- presence/absence of a species
- co-existence of several species
- abundance of a species

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16
Q

How does geochronology date rocks

A

Use of radioactive decay, where a parent isotope decays into daughter isotopes and releases neutrons.
N=No*e^lamda(t)
- Daughter composition usually different to adult
Radioactive clock measures time of crystallisation
- Need to assume a closed system

17
Q

What is isotope stratigraphy

A
  • elements and their isotopes are cycled through crust, hydrosphere, atmosphere and biosphere
  • isotope ratios vary over time in response to environmental, crustal and biological changes
  • where changes are globally synchronous, can be applied to isotope stratigraphy
  • isotope ratios have further applications in palaeoclimate reconstructio, diagenesis, igneous and metapmorphic petrogenesis
18
Q

What is Magnetostratigraphy?

A

Remnant magnetism (natural alignment of magnetic minerals above the curie point ~570c is preserved when cooled), shows orientation of earths magnetic dipole at time of cooling