Stratigraphy Flashcards
The study of temporal and spatial relationships between bodies of sedimentary rocks.
Stratigraphy
What is the goal of stratigraphic analysis?
To establish the temporal sequence of
sedimentary rocks in the area under investigation.
Principles of Stratigraphy
Law of Superposition
Law of Original Horizontality
Lateral Continuity
Cross-Cutting Relationships
Inclusion
Unconformity
Law of Faunal Succession
The oldest layer is at the base and that the layers are progressively younger with ascending order in the sequence.
Law of Superposition
All rock layers are originally laid down (deposited) horizontally and can later be deformed.
Law of Original Horizontality
All rock layers are laterally continuous and may be broken up or displaced by later events.
Lateral Continuity
Younger rocks cut across older rocks.
Cross-Cutting Relationships
Any rock fragments that are included in rock must be older than the rock in which they are included.
Inclusions
Represents a long period during which deposition ceased, erosion removed previously formed rocks, and then deposition resumed. In each case, uplift and erosion are followed by subsidence and renewed sedimentation.
Unconformity
States that a species appears, exists for a time, and then goes extinct. Time periods are often recognized by the type of fossils you see in them.
Law of Faunal Succession
Determining a sequence of events occurred in the history of earth using the evidence of organic evolution in the sedimentary rocks accumulated through geologic time.
Dating
It is when rocks and events are put in correct order of sequence relative to one another.
Relative Dating
The age of rocks units are determined precisely in years using the rate of decay of naturally occurring radioactive elements.
Absolute Dating
Usually a product of interpretation of other stratigraphic analysis of the basin.
Chronostratigraphy
Its ultimate aim is to arrange the sequence of deposition and the time of deposition of all rocks within a geological region.
Chronostratigraphy