Introduction and stratigraphic methods Flashcards
What can stratigraphy be used for?
Determining tectonic, biological, and climatic events
What are the two ways to determine geological age?
Relatively or numerically
Define relative geological aging
Placing rocks and events in their proper sequence of formation/occurence
Lithostratigraphy
Define numerical (absolute) geological aging
Specifying absolute number of years since an event
Geochronology
Describe the principle of superposition
Relative aging
Each bed is younger than the one below it
Thrust faulting can invert the order
Describe the principle of cross-cutting
Relative aging
A bed or unit is younger than the one it cuts across
Describe the principle of original horizontality
Relative aging
Consolidated strata that are now tilted were originally deposited horizontally
Describe the principle of continuity
Relative aging
In a basin, the same bed is of identical age in every part, beds terminate were deposition was not possible or where they have been eroded or deformed after deposition
Describe the principle of inclusion
Relative aging
If an element A is included in an element B, A is older than B
Describe palaeontological identity
Relative aging
All beds including the same fossils are of the same age
Relies of the principle of faunal succession
Not applicable where there has been reworking
Describe an unconformity
Relative aging
A break in the geological record produced by erosion and/or non-deposition
Describe an angular unconformity
Relative aging
Tilted rocks are overlain by flat-lying rocks
Describe a disconformity
Relative aging
Strata on either side a parallel, there have been a period of erosion
Describe a non-conformity
Relative aging
Metamorphic or ignous rocks in contact with sedimentary strata
Describe isotopic ratios
Relative aging
Applicable when changes are globally synchronous
O2 linked to temp
C linked to biological activity
S linked to igneous processes
Correlates within basin
Supported by absolute age dates