Introduction Flashcards

1
Q

Tectonics

A

structure and tectonics interact, cant draw a line between them

tectonics are external processes that cause a characteristic set of structures in an area

plate tectonics

salt tectonics

neotectonics
- crustal motions and contemporaneous stress field

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2
Q

plate tectonics

A
  • movement and interaction of lithospheric plates
    there are major and smaller plates
    plate boundaries join to form a network
    example of subduction ->indian plate started to collide with Asia about 15 million years ago
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3
Q

salt tectonics

A

salt is a rock
- deformation from vertical movement of salt through its overburden
-layers of salt cut through the sedimentary layers above them
-salt is not permeable

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4
Q

deformation

A

conglomerate (large clasts, matrix supported) -> clasts can get flattened or stretched

different rocks behave differently under the same conditions
->not all rocks deform in the same way under the same chemical an physical conditions

the same rock will behave differently depending on the chemical and physical conditions (HPT vs LPT)

usually high pressure and high temperature go together ->not always

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5
Q

stress

A

stress on a plane is the force per unit area of the plane

stress = force/area

the same force applied on a smaller area will cause more damage

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6
Q

deformation and strain

A

any change in shape/distortion (strain), position (translation), or orientation (rotation) of a body under stress
3 components: rotation, translation, and strain

as long as a rock has one of three components, you can say it is deformed

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7
Q

homogeneous vs inhomogeneous (heterogeneous)

A

homogeneous -> everything has moved/been changed in the same way

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8
Q

factors that affect deformation

A

different rock types (chemical/mineralogical composition)
->have different chemical properties

physical and chemical environments

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9
Q

main types of structures

A

Non-tectonic (primary)
->not due to deforming forces
->formed during the formation of the rock

Tectonic (secondary)
1. Brittle structures
2. Ductile structures

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10
Q

types of tectonic structures

A

brittle -> loss of cohesion

ductile -> no loss of cohesion

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11
Q

scale of observations

A

microscopic
-> only visible under thin section

mesoscopic
-> can be observed directly
-> from hand samples to large, continuous outcrop

macroscopic
-> several outcrops to whole mountain ranges
-> cant be observed directly, need interpretation

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12
Q

methods in structural geology

A

fieldwork - most essential

other techniques - data and modelling, measuring crystallographic orientation of constituent crystals, look at structural details within individual crystals

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13
Q

structural analysis

A

2 distinct steps:

  1. study and description of a rock in its present state

2.

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14
Q

geometric analysis

A

geometrical features are studied
infer what the geometry is, descriptive, free from reference

characterization of the form, extent, and arrangement of structures in a map area

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15
Q

kinematic analysis

A

from the results of the geometrical analysis
-> attempt to reconstruct movements that took place during the deformation of the rock
-> rotation, translation, strain

how the geometric formed

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16
Q

dynamic analysis

A

what kind of forces led to the movement & formation of the structures

17
Q

tectonic analysis

A

Uses data (structural, stratigraphic, etc.) to analyze the tectonic processes that were involved in the geological evolution of an area

ie. how did tectonic processes contribute to the current geology of an area