Relative Time Scale Flashcards

1
Q

Define Biostratigraphy

A

About layers of specific beds of rock

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2
Q

Define chronostratigraphic

A

Chronostratigraphic correlation matches rocks of the same age, even though they are made of different lithologies. Different lithologies of sedimentary rocks can form at the same time at different geographic locations because depositional environments vary geographically

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3
Q

Define stratigraphy and its principles

A

Principle of Super position
Principle of original horizantality
principle of lateral continuity
Is the study of layerd sedimentary rocks

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4
Q

Define principle superposition

A

In an otherwise undisturbed sequence of sedimentary strata, or rock layers, the layers on the bottom are the oldest and layers above them are younger.

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5
Q

Principle of original horizontality

A

Layered rocks are generally laid down flat at their formation.

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6
Q

Principle of lateral continuity

A

Layered rocks can be assumed to continue if interrupted within its area of deposition.

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7
Q

Relative time dating princples

A

Principle of Cross-Cutting relationships
Principle of Inclusions
Principle of Fossil Succession

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8
Q

Angular disconformity ** mid term question, on the previous midterm. Grand Canyon

A

Two rock layers that have different angles of deposition relative to horizontal.
The Phanerozoic strata in most of the Grand Canyon are horizontal. However, near the bottom horizontal strata overlie tilted strata. This is known as the Great Unconformity and is an example of an angular unconformity. The lower strata were tilted by tectonic processes that disturbed their original horizontality and caused the strata to be eroded. Later, horizontal strata were deposited on top of the tilted strata creating the angular unconformity

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9
Q

How does intrusive igenous rocks play into relative time

A

a

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10
Q

Define Dike

A

A narrow igneous intrusion that cuts through existing rock, not along bedding planes.

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11
Q

Define sill

A

A type of dike that is parallel to bedding planes within the bedrock.

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12
Q

Define principle of inclusion

A

Primarily for sedimentary rocks, check text

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13
Q

Define Principle of Fossil Succession

A

stratiphed rocks of different layers, have different fossils and evolutionary organisms in them.

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14
Q

Define Detrital zircons

A

Detrital sedimentary rocks are less useful because they are made of minerals derived from multiple parent sources with potentially many dates. However, scientists can use igneous events to date sedimentary sequences

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15
Q

define disconformity

A

wo layered rocks that may seem conformable, but an erosional surface exist between them.

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16
Q

Define nonconformity

A

Layered rocks on top of a non-layered rock, such as crystalline basement.

17
Q

Define unconformities

A

Missing time in the rock record, either because of a lack of deposition and/or erosion.

18
Q

Principle of lithostratigraphic

A

Lithostratigraphic correlation establishes a similar age of strata based on the lithology that is the composition and physical properties of that strata.