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Chapter 10 Geologic
Time
10-1 A brief history:
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Catastrophism: the earth's feature is creased by unknown
forcers, not operating now.
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Uniformitarianism: the laws governing today are also the
laws governing in the past. It was proposed by Hutton, successfully
interpreted by Lyell. Some animals and plants live in water, indicating they
lived in water when their fossils were found.
10-2 Relative dating:
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For a sequence of rock formation, which formed first, which
second, etc.
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Doesn't tell exactly when why formed.
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Law of superporition: Proposed by Nick Steno. In undisturbed
formation, the lower the formation, the older the formation (Fig. 10.3B).
How do we know that the figure is not upside down?
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Principle of original horizontality: states when the rocks
formed, the formation was horizontal.
Cross-cutting relationship: sequence of formation in Fig
10.5:
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Sandstone formation
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Fault A
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Conglomerate
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Fault B
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Batholith
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Dike B
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Dike A
The one that cuts through other formations is younger.
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Inclusions: Fig. 10.10.
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Unconformities: represents time lapse between the two
formation, indicating weathering occurred.
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Angular unconformity: the older and younger formation
don't have same tilting angles.
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Disconformity: time gaps exist, but both formations have
same angles.
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Nonconformity: contact between sedimentary and igneous
or metamorphic rocks. Fig. 10.7.
10-3 Correlation of rock layers using
fossils:
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Fossils:
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Types of fossils:
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Bones, teeth, shells, easy to be petrified.
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Others: impression, tracks, borrows (tubes made by
animals), foot prints.
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Animal fossils vs. plant fossils.
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Fossil succession:
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Index fossils: fossils occurred in larger area but a short
period of time. Index fossils are used to match rocks with similar ages.
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Other information fossils provide:
10-4 Absolute dating:
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Atoms composed of nucleus and electrons, nucleus composed of
protons and neutrons. Charges each type of particles provide: protons: +,
neutrons: none, electrons: -. For an atom, electric charge is neutral.
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Different atoms have different numbers of protons, e.g. 126C,
and 147N.
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If the numbers of p the same and the numbers of n
different, they are called isotopes, e.g. 126C, 136C,
and 146C.
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Stable vs. radioactive isotopes:
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Types of radioactive decay:
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alpha-particles, 2n + 2p released,
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beta-particles, an electron emitted.
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electron capture: an electron is gained.
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Half-life: Time required to decay half of the original
nucleus.
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Common radionuclides for dating geologic rocks: K/Ar, Rb/Sr,
and U/Pb for loder rocks and 14C for younger rocks.
10-5 Geologic time scale:
Used to be on relative scale. Now absolute scale is added.
1. Eon: the largest division:
2. Ears: one scale smaller than Eon.
| Cenozoic |
| Mesozoic |
| Paleozoic |
3. Period: one scale smaller than Eras:
| Q quaternary |
| T tertiary |
| K Cretaceous |
| J Jurassic |
etc.
4. Epoch: Early, middle, and late
Notice the division: The older, the wider. Why? Not enough
information to accurately date.
10-6 Difficulties in dating:
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Absolute dating works better for crystalline rocks, not
for sedimentary rocks, e.g. K/Ar in mica. If the mica was in sedimentary
rocks, the mica was formed much earlier than the sedimentary rock.
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Combination of relative sequence with absolute dating
works best, e.g. Fig 10.18. The igneous dike was dated 66 Ma, the Mancos
shale formation formed should be before 66 Ma.
Homework:
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Read chapter summary on p.291.
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Use your own word to explain the key terms on page 291.
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Answer the review questions on page 292.
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