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28 Cards in this Set

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What is active geophysical methods

Active methods artificially produce an electrical, electromagnetic, or acoustic signal that is transmitted into the ground. Variations in the subsurface interact with and modify these signals according to their specific physical properties, producing an altered return signal that is measured by instrumentation at the surface. Resistivity methods inject an electrical current, soil conductivity meters transmit radio energy, and ground penetrating radar sends a microwave pulse; in each case the instrumentation measures a response to these actions.

What is passive geophysical methods

Passive methods detect variations within the natural fields of the earth. They include magnetic and gravitational fields, and certain native electrical properties within the soil. Magnetometry is the principal passive method employed in archaeo-geophysics.

What are the three sources for the magnetic field that we measure at Earth’s surface and what are the timescales of variation for each?

1) external field: from the magnetosphere (minutes to days)



2) internal core field: from dynamo action in the outer core (years to geologic time scales)



3) crustal field: from remenant magnetization (geologic time scales)

How do we describe magnetic field or magnetization?

Magnetic field is a vector and as such it has both a direction and an intensity. At any point, the field can be described by declination, inclination and intensity.

What is Declination?

Angular deviation from true north in the horizontal plane

What is Inclination?

angular deviation from horizontal (defined as positive down)

What is Intensity?

the strength or magnitude of the field

What is the Geocentric Axial Dipole (GAD) assumption?

The approximate dipole is located at the center of the Earth and aligned with the Earth’s spin axis.

If we assume GAD, how does inclination vary with latitude?

actual inclination does not exactly match the dipole equation

Why does Earth’s field deviate from GAD over short time scales?

Earths dipole flips

What is Diamagnetism?

Precession of electrons in the presence of a magnetic field. Generates a field appeasing the inducing field.

What is Paramagnetism?

Becomes magnetized in the presence of a field, but magnetization is zero in the absence of a field. It has no remanent magnetization.

What is Ferromagnetism?

Retains a magnetization even in the absence of a field. Has remanent magnetization.

What is Remanent magnetization?

the (permanent) magnetization present in a material

What is Induced magnetization?

is the (temporary) magnetization present in a material only as long as a field is applied.

What are 4 processes by which rocks can become permanently magnetized?

1) thermo remanent
2) detrital remanent
3) isothermal remanent
4) chemical remanent

What is thermo remanent magnetization?

a magnetization acquired on cooling through a rock's Curie temperature(s) and blocking temperatures

What is detrital remanent magnetization?

a magnetization acquired by sediments during deposition

What is isothermal remanent magnetization?

re/magnetization in the presence of a large magnetic field, such as a lightning bolt strike

What is chemical remanent magnetization?

magnetization acquired when a magnetic crystal forms in a magnetic field below its Curie temperature.

What is the fold test? Baked contact test? Conglomerate test?

Tests to find out when magnetization was acquired before or after folding, before or after intrusion, before or after emplacement of conglomerate.

What is a virtual geomagnetic pole (VGP) and how is it related to apparent polar wander?

The point on the Earth's surface at which a magnetic pole would be located if the observed direction of remanence at a particular location was due to a magnetic dipole at the centre of the Earth.

What is apparent polar wander?

the perceived movement of the Earth's paleo-magnetic poles relative to a continent while regarding the continent being studied as fixed in position.

When we measure magnetic anomalies produced by a magnetic body below Earth’s surface, how and why do we care about the direction of Earth’s field at our measurement location?

We measure magnetic anomalies as deviations from the surrounding (ambient) Earth’s field. We must know direction of Earth’s field at our measurement location in order to calculate the anomaly.

Imagine that Earth's field is (largely) caused by a bar magnet in the center of the Earth. Let's refer to magnetic north as the location where this imaginary bar magnet would pierce Earth's surface. What is the present angular difference between true north (Earth's spin axis) and magnetic north?


11.5°

If the Earth's field could be represented by a perfect dipole (like a bar magnet), inclination would vary smoothly from equator to pole. What would the inclination be at the following latitudes (45°N, North Pole, Equator).

45°N = +63° inclination
North pole (+90°) = +90° inclination
Equator (0°) = 0° inclination

Paleomagnetism involves..

rocks that retain a magnetism acquired long ago

True or False - Magnetite has a stronger magnetic remanence than hematite?

True