Stratigraphy Flashcards

1
Q

The study of temporal and spatial relationships between bodies of sedimentary rocks.

A

Stratigraphy

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2
Q

What is the goal of stratigraphic analysis?

A

To establish the temporal sequence of
sedimentary rocks in the area under investigation.

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3
Q

Principles of Stratigraphy

A

Law of Superposition
Law of Original Horizontality
Lateral Continuity
Cross-Cutting Relationships
Inclusion
Unconformity
Law of Faunal Succession

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4
Q

The oldest layer is at the base and that the layers are progressively younger with ascending order in the sequence.

A

Law of Superposition

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5
Q

All rock layers are originally laid down (deposited) horizontally and can later be deformed.

A

Law of Original Horizontality

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6
Q

All rock layers are laterally continuous and may be broken up or displaced by later events.

A

Lateral Continuity

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7
Q

Younger rocks cut across older rocks.

A

Cross-Cutting Relationships

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8
Q

Any rock fragments that are included in rock must be older than the rock in which they are included.

A

Inclusions

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9
Q

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.

A

Unconformity

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10
Q

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.

A

Law of Faunal Succession

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11
Q

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.

A

Dating

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12
Q

It is when rocks and events are put in correct order of sequence relative to one another.

A

Relative Dating

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13
Q

The age of rocks units are determined precisely in years using the rate of decay of naturally occurring radioactive elements.

A

Absolute Dating

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14
Q

Usually a product of interpretation of other stratigraphic analysis of the basin.

A

Chronostratigraphy

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15
Q

Its ultimate aim is to arrange the sequence of deposition and the time of deposition of all rocks within a geological region.

A

Chronostratigraphy

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16
Q

Uses fossils to establish relative ages of rock and correlative successions of sedimentary rocks within and between depositional basins.

A

Biostratigraphy

17
Q

Fossils used in petroleum industry?

A

Microfossils
Nanofossils
Palynomorphs

18
Q

An interval of geologic strata characterized by certain fossil taxa.

A

Biozone

19
Q

Relies on the correlation of rocks of the same characteristics. Most maligned stratigraphic method and also the oldest of them all.

A

Lithostratigraphy

20
Q

The study of seismic data for the purpose of extracting stratigraphic information.

A

Seismic/Tectonic Stratigraphy

21
Q

Generated by the accumulation of sediments in a basin wherein major changes brought about by the tectonics in the area affects the gross structure of sediment package.

A

Seismic/Tectonic Stratigraphy

22
Q

What are the different margins identified by tectonic stratigraphy?

A

Reef Basins
Passive Margin
Foreland Basins
Wrench Systems

23
Q

Packages of sediment deposited before, during, and after the active rift phase can often be clearly identified on regional seismic lines.

A

Reef Basins

24
Q

A development of a successful rift. It can develop over a substantial period of time, thus, the megasequence can be enormously thick

A

Passive Margins

25
Q

Forms contemporaneously with the flexuring of the lithosphere caused by thrust loading. The shape is commonly elongate parallel to the thrust belt.

A

Foreland Basins

26
Q

Megasequences developed during strike-slip are commonly of small aerial extent. The sequences may be symmetric, as in transtensional systems, or asymmetric, as in transpressional systems. The overall geometry of the megasequences is commonly like that of their syn-rift and foreland counterparts in extensional and compressional basins.

A

Wrech Systems

27
Q

Involves the geochemical classification and correlation of sedimentary strata by using major and trace element geochemistry, which is highly helpful when applied to sequence with poor biostratigraphic control.

A

Chemostratigraphy

28
Q

A geophysical correlation technique used to date sedimentary and volcanic sequences. The method works by collecting oriented samples at measured intervals throughout the section and analyzing the magnetic polarity of each sample.

A

Magnetostratigraphy

29
Q

A branch of sedimentary stratigraphy that deals with the order or sequence in which depositionally related stratal successions (time-rock) units were laid down in the available space or accommodation. It is developed from seismic stratigraphy.

A

Sequence Stratigraphy

30
Q

A geologic event in which sea level rises relative to the land and the shoreline moves toward higher ground, resulting in flooding. It can be caused by either the land sinking or the ocean basin filling with water.

A

Transgression

31
Q

With a rise in sea level, we see a landward shift of facies zones and the stratigraphic section reveals the texture is fine upward.

A

Transgression

32
Q

A geological process occurring when areas of submerged seafloor are exposed above the sea level. A marine regression when sea level is falling.

A

Regression

33
Q

With a fall in sea level, we see a seaward shift of facies zones and the stratigraphic section reveals that texture coarsens upward

A

Regression