What are the 5 principles of Stratigraphy
Principle of Superposition
Principle of Original Horizontality
Principle of Cross-Cutting relations
Principle of Inclusions
Principle of Fossil Succession
Describe the Principle of Superposition
In an undisturbed sequence of rocks, the oldest rocks are at the bottom and the youngest at the top. If it is found to be the reverse, the sequence must have been overturned at some point
Describe the principle of Cross-Cutting Relations
If a rock unit is cross-cut by another feature such as a fault or igneous intrusion, the feature that cuts across is younger than the rock unit which is dissected
Describe the Principle of Original Horizontality
All waterline sediments were deposited horizontally (or nearly so). If sedimentary rocks are found tilted or overturned, this was due to a later event. This principle only determines the relative time of the tilting event (often the tilting is due to the beds being part of large scale folds)
Describe the principle of Inclusions
When a rock unit contains fragments of another rock within it, those fragments represent a rock that is older than the rock around them.
Describe the principle of fossil succession
Fossil species follow each other in the rock record in a recognizable and irreversible order. Thus we can use this information to correlate strata over large distances, despite differences in rock type of geologic processes.
What are unconformities
Much of geologic time in a given region is not included in the rock record. Theses are times in which the erosion was occurring rather than deposition. We would expect to see rocks of a certain age, but don’t. What we do see is an erosional surface of older rock overlain by younger sediments called an unconformity.
What are the 3 main types of unconformity
Angular unconformity
Disconformity
Nonconformity
What is an Angular Unconformity
An erosional surface between older layers which have been uplifted and tilted prior to erosion, and younger layers. A different dip angle between the overlying and underlying beds results.
What is a disconformity
The older, eroded surface is made of sedimentary layers which have the same orientation as the overlying beds. This type is the most difficult to see in the field and requires a thorough knowledge of local geology, often based on missing fossil sequence.
What is a nonconformity
Older, eroded surface is a crystalline rock which is subsequently overlain by sediments. Only contacts between igneous rocks and overlying rocks that are erosional are nonconformities.
What are radioactive isotopes
Radioactive isotopes are elements in minerals that are able to tell us how much time has elapsed since the rock was formed. This is because radioactive isotopes are unstable and decay or break down at predictable rates.
What is an isotope
An isotope is one of several forms of one element, all having the same number of protons in the nucleus, but differing in the number of neutrons
What is Radiometric dating
Radiometric dating is possible because radioactive atoms of some elements are incorporated into the crystal lattice of minerals at the time of their formation. Over time these parent atoms decay and their daughter elements are trapped within the mineral.
What level does radioactive decay occur on
Radioactive decay occurs on the atomic level as particles in the nucleus disintegrate, changing the atom into one of a different element and emitting radiation in the process.
What is a half life
The half life is the time it takes half a sample of a radioactive isotope to decay. Constant no matter the amount of the isotope. So the time it takes to go from 100% to 50%, is equal to the time it takes to go from 50% to 25%.
What is decay curve
A decay curve is a simple graph that represents the amount of parent isotope we would expect to find remaining in a mineral or rock after a given period of time has passed.
What formula gives the percentage of parent atoms remaining after time n
2^-n
What is the detection limit for most radioactive elements
The detection limit for most radioactive elements rarely exceeds five half lives
What is the decay of U238
U238 -> Pb206
HL = 4.56 BY
Found in Zircons (in granites) and uranitite
What is the decay of U235
U235 -> Pb207
HL = 704 MY
found in Zircons (in granites), and uranitite
What is the decay of K40
K40-> Ar40 and Ca40
HL = 1.251 BY
Found in muscovite, biotite, hornblende, K-feldspar, glauconite, volcanic rock
What is the decay of Rb87
Rb87->Sr87
HL = 48.8 BY
Found in K-mica, K-felspar, Biotite, metamorphic rocks
What is the decay of Th230
Th230->Pb206
HL = 75 KY
Found in Oceanic Sediments