Week2 D3 Flashcards

1
Q

The theory states that new lithosphere is formed at ocean ridges due to the uplift of mantle material and moves away until it collides with another plate and subduct. The motion is described to me similar to a conveyor belt.

A

Plate Tectonics

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2
Q

The theory was proposed to explain magnetic anomalies on the sea floor

A

Seafloor spreading

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3
Q

Accretionary plate boundaries where new lithosphere is formed from upwelling mantle

A

Ocean Ridge

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4
Q

Average rate of production of oceanic lithosphere

A

3.5 km^2/yr

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5
Q

A seismic region that descends beneath a continental margin or an island arc, with a deep-sea trench serving as its visible manifestation on the surface.

A

Benioff Zone

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6
Q

Most common type of tranform fault

A

Ridge-Ridge

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7
Q

This concept is used to describe motions on the surface on the sphere

A

Euler’s ‘fixed-point’ theorem

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8
Q

This law describes the connection between the trajectory of a light ray as it traverses the boundary or interface between two adjacent substances and the refractive index of each substance involved.

A

Snell’s Law

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9
Q

measuring the precise position of sites on the Earth’s surface from sources in space, such as radio-wave sources and satellite tracking

A

Space Geodesy

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10
Q

Is a type of force that pulls the body apart

A

Tensional

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11
Q

two opposite forces that act upon the same object, but not along the same line

A

Shear Forces

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12
Q

External forces that tend to compress

A

Compresisonal

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13
Q

Types of deformation

A

Plastic

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14
Q

Formula for Young’s Modulus

A

Tensile stress/Tensile Strain

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15
Q

Formula for Shear Modulus

A

Shear Stress/Shear Strain

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16
Q

Rigid body deformation is categorized into

A

Translation and Rotation

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17
Q

What are the basic premises in plate tectonics

A

> Lithosphere is a rigid and strong substancer resting on a weaker plastic region called asthenosphere
Lithosphere is broken into several segments known as plates

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18
Q

Four types of seismic boundaries based on epicenter distributions and geologic characteristics

A

Ocean Ridges, Subduction Zones, Transform Faults and Collisional Zones

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19
Q

Seven Major Plates

A

Eurasion, Antarctic, N. American, S. American, Pacific, African, and Australian Plates

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20
Q

Examples of Intermediate plates, give 3

A

Philippine, Arabian, Nasca, Cocos, Carribean, Scotia Plates

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21
Q

Examples of Small plates, give 3

A

Turkish-Aegean, Adriatic, Arabian, Iran Plates

22
Q

Two Types of continental margins

A

Active continental margins and Passive continental Margins

23
Q

Active vs Passive continental margins

A

Active Continental Margin: subduction zone or a transform fault coincides with continent-ocean interface.
Passive Continental Margin: along edges of basins where little to no tectonic activity is seen

24
Q

Difference betwwen fast and slow spreading ridges in terms of axial topography

A

Fast Spreading ridges: low relief; some intances of topographic highs
Slow Spreading ridges: deep axial valley, flanking mountains

25
Q

What are transform faults

A

plate boundaries where they slide past each other and plate surface is more or less conserved

26
Q

Three types of Transform faults

A

Ridge-Ridge, Trench-Trench, Ridge-Trench Faults

27
Q

The formula for getting the relative velocy (v) between two plates

A

v = ωR sin θ [ ω = angular velocity, R = earth’s radius, θ is the angular distance between the rotation pole P and a certain point]

28
Q

Give the chemical equation for the conversion of microcline to kaolinite

A

2 KAlSi3O8 + 9H2O + 2H <=> Al2Si2O5(OH)4 +2K + 4H4SiO4

29
Q

What are the mechanism that drives plate movement

A

Slab pull and Ridge Push

30
Q

Non rigid body deformation is categorized into

A

Distorsion, Dilation

31
Q

What is Young’s modulus

A

The property of a material pertaining to how easily it can strech and deform.

32
Q

What is the definition of Shear Modulus

A

Measures the resistance of a material to change shape, usually applied for shear stress

33
Q

What is Poisson’s Ratio

A

the ratio between the strain in width vs length; pertains to the overall strain of a material

34
Q

What is the Bulk Modulus or Incompressibility

A

a measure of a material’s resistance to compression

35
Q

What does INSAR stand for

A

Interferometric Synthetic Aperture Radar

36
Q

Why doesnt the earth grow despite the production of new crust at ocean ridges

A

As new crust is produced from the upwelling of magma at oceanic ridges, old oceanic crust is destroyed as they subduct to the mantle.

37
Q

Illustrate the geometry of RRR triple junction

A

Illustration at physical copy

38
Q

Illustrate the geometry of TTT triple junction

A

Illustration at physical copy

39
Q

Illustrate the geometry of TTF triple junction

A

Illustration at physical copy

40
Q

Illustrate the geometry of FFR triple junction

A

Illustration at physical copy

41
Q

Illustrate the geometry of FFT triple junction

A

Illustration at physical copy

42
Q

Illustrate the geometry of RTF triple junction

A

Illustration at physical copy

43
Q

Illustrate the six types of transform fault

A

A. Ridge-Ridge
B and C. Ridge-Trench
D, E and F. Trench-Trench

44
Q

Breifly explain and Illustrate the Wilson Cycle

A

The repetitive process of ocean basins opening and closing is attributed to the Earth’s plate movements. The Wilson cycle commences with the emergence of a magma plume and the subsequent thinning of the overlying crust. As extensional tectonic forces persistently thin the crust, an ocean basin takes shape, and sediments gather along its borders. Eventually, subduction begins at one of the ocean basin’s edges, leading to the closure of the basin.

45
Q

What would be the relative velocity of Plate B, based from an observer standing on Plate C?

A

Illustration at physical copy

46
Q

How high does a 70km-thick crust stick out above the mantle

A

Illustration at physical copy

47
Q

Assume the mechanism for co-seismic defomation at the PFZ is simple shear. A certain region affected by shearing extends for 80 km on either side of the fault and the average displacement parallel to the fault is 6 m. Calculate the shear strain

A

Illustration at physical copy

48
Q

Why is plate tectonics an important theory in Geology?

A

The concept of plate tectonics is a unifying theory that explains much of earth’s processes.

49
Q

Can tranform faults produce new crust, if so then how?

A

Oceanic transform fault boundary are “leaky” where magma escapes from such boundaries producing slivers of lithosphere

50
Q

Why is it that hypocenters are only found until 660 km depth?

A

Beyond the 660 km dpeth lies the asthenosphere. Since the layer is plastic in nature, brittle deformation cannot happen since its response would be ductile. This earthquakes does not occur beyond these depths.