Upload
garry-hawkins
View
231
Download
0
Tags:
Embed Size (px)
Citation preview
1
Chapter 8
Time and Geology
GEOL 101
Introductory Geology
2
Determining Geological Ages
Relative age dates – placing rocks and events in their proper sequence of formation
Numerical (absolute age) dates – specifying the actual number of years that have passed since an event occurred
3
Principles of Relative DatingLaw of superposition
• Undeformed section of sedimentary or layered igneous rocks
• Oldest rocks are on the bottom
Principle of original horizontality• Layers of sediment are generally deposited
in a horizontal position• Rock layers that are flat have not been
disturbed (deformed)
Principle of cross-cutting relationships• Younger features cut across older features
4
Superposition Strata in the Grand Canyon
5
Horizontality
6
Cross-cutting Relationship
7
Cross-cutting Relationship
Which crater is youngest?
8
Cross-cutting Relationships
9
Principles of Relative Dating
Inclusions
A piece of rock that is enclosed within another rock
Rock containing the inclusion is younger
Unconformity
Break in rock record produced by erosion and/or nondeposition of rock
Represents period of geologic time
10
Principles of Relative Dating
Types of unconformities• Angular unconformity – tilted rocks
(disturbed) are overlain by flat-lying rocks
• Disconformity – strata on either side of the unconformity are parallel
• Nonconformity – metamorphic or igneous rocks in contact with sedimentary strata
11
Angular Unconformity
12
Angular Unconformity
13
Angular Unconformity
Animation
14
Disconformity
15
Disconformity
16
Nonconformity
17
Nonconformity
18
Nonconformity
Inclusions
19
Grand Canyon Unconformities
20
Interpret Geologic HistoryAnimation
21
Correlation of Rock Layers
Matching of rocks of similar ages in different regions is known as correlation
Correlation often relies upon fossils• similar sedimentary strata in widely
separated areas• identified and correlated by distinctive
fossil content• Principle of fossil succession
– fossil organisms succeed one another in a definite and determinable order
– time period recognized by its fossil content
22
Correlation of Rock Layers
23
Fossils Ages of Rocks
24
Radioactivity: spontaneous changes (decay) in the structure of atomic nucleiBasic atomic structureTypes of radioactive decayParent, daughter product, half-lifePrinciple of radioactive datingSources of errorCarbon-14 (radiocarbon) datingImportance of radiometric dating
Radiometric Dating
25
Basic Atomic Structure• Nucleus
– Protons: positively charged particles with mass– Neutrons: neutral particles with mass– Electrons: negatively charged particles, orbit nucleus
• Atomic number– An element’s identifying number– Number of protons in the atom’s nucleus
• Mass number– Sum of protons & neutrons in atom’s nucleus
• Isotope– Variant of the same parent atom– Differs in the number of neutrons– Different mass number than the parent atom
26
Types of radioactive decay• Alpha emission
– Emission of 2 protons & 2 neutrons (alpha particle) – Mass number is reduced by 4 and the atomic
number is lowered by 2• Beta emission
– Electron (beta particle) is ejected from the nucleus– Mass number remains unchanged and the atomic
number increases by 1• Electron capture
– Electron is captured by the nucleus– Electron combines with a proton to form a neutron– Mass number remains unchanged and the atomic
number decreases by 1
Radiometric Dating
27
Radiometric Decay
Electron Capture
AlphaEmission
BetaEmission
28
Parent – an unstable radioactive isotope
Daughter product – the isotopes resulting from the decay of a parent
Half-life – the time required for one-half of the radioactive nuclei in a sample to decay
Radiometric Decay
29
Uranium Isotopes
ParentU238
DaughterPB206
Atomic # - 92Mass # - 238
Atomic # - 82Mass # - 206
30
Principle of radioactive dating• The percentage of radioactive toms that
decay during one half-life is always the same (50 percent)
• However, the actual number of atoms that decay continually decreases
• Comparing the ratio of parent to daughter yields the age of the sample
Radiometric Dating
31
Radioactive Decay Curve
32
Radioactive Decay Curve
33
Radiometric Dating
34
Sources of error• A closed system is required• To avoid potential problems, only fresh,
unweathered rock samples should be used
Carbon-14 (radiocarbon) dating• Half-life of only 5730 years• Used to date very recent events• C14 is produced in the upper atmosphere
Radiometric Dating
35
C14 Production and Decay
Neutron Capture
BetaEmission
36
Importance of radiometric dating• Radiometric dating is a complex
procedure that requires precise measurement
• Rocks from several localities have been dated at more than 3 billion years
• Confirms the idea that geologic time is immense
Radiometric Dating
37
Other Dating Methods
Shell GrowthRings
TreeRings
Rhythmic Layering in Glaciers
38
Cross-Dating Principle in Dendrochonology
Youngest Older
Oldest
39
Geologic Time Scale
Geologic time scale – Earth history calendar • Subdivides geologic history into units• Originally created using relative dates
Structure of the geologic time scale• Eon – the greatest expanse of time
– Phanerozoic – “visible life”, most recent eon
– Proterozoic – before life
– Archean – ancient
– Hadean – mythical subterraneon world of departed spirits, oldest eon
– Precambrian: Proterozoic, Archean, Hadean
40
Geologic Time ScaleEra – subdivision of an eon
Precambrian – no era subdivisions
Eras of the Phanerozoic eon• Cenozoic (“recent life”)• Mesozoic (“middle life”)• Paleozoic (“ancient life”)
Eras are subdivided into periods
Periods are subdivided into epochs
41
Geologic Time Divisions
42
Geologic Time Scale
43
Geologic Time ScalePrecambrian time
• Nearly 4 billion years prior to the Cambrian period
• Not divided into smaller time units because the events of Precambrian history are not know in great enough detail
– First abundant fossil evidence does not appear until the beginning of the Cambrian
Visualizing vast period of geologic time
44
Evolution vs Geologic Time
45
Visualizing Geologic Time
Twice around the equator
46
Geologic Time Scale Difficulties• Not all rocks can be dated by radiometric
methods– Grains comprising detrital sedimentary rocks are
not the same age as the rock in which they formed– The age of a particular mineral in a metamorphic
rock may not necessarily represent the time when the rock formed
• Datable materials (such as volcanic ash beds and igneous intrusions) are often used to bracket various episodes in Earth history and arrive at ages
47
Sedimentary Ages using Radiometric Dating
48
Stratigraphic Dating