Encyclopedia of Geomagnetism and Paleomagnetism
(Sprache: Englisch)
Consisting of more than 300 articles, this is the first single encyclopedia to encompass the fields of Geomagnetism and Paleomagnetism in a single volume. It details the current state of knowledge and provides an up-to-date synthesis of the most basic concepts.
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Consisting of more than 300 articles, this is the first single encyclopedia to encompass the fields of Geomagnetism and Paleomagnetism in a single volume. It details the current state of knowledge and provides an up-to-date synthesis of the most basic concepts.
Klappentext zu „Encyclopedia of Geomagnetism and Paleomagnetism “
This reference encompasses the fields of Geomagnetism and Paleomagnetism in a single volume. Both sciences have applications in navigation, in the search for minerals and hydrocarbons, in dating rock sequences, and in unraveling past geologic movements such as plate motions they have contributed to a better understanding of the Earth. The book describes in fine detail the current state of knowledge and provides an up-to-date synthesis of the most basic concepts. It is an indispensable working tool not only for geophysicists and geophysics students but also for geologists, physicists, atmospheric and environmental scientists, and engineers.
Understanding the process underlying the origin of Earth magnetic field is one of the greatest challenges left to classical Physics. Geomagnetism, being the oldest Earth science, studies the Earth's magnetic field in its broadest sense.
The magnetic record left in rocks is studied in Paleomagnetism. Both fields have applications, pure and applied: in navigation, in the search for minerals and hydrocarbons, in dating rock sequences, and in unraveling past geologic movements such as plate motions they have contributed to a better understanding of the Earth.
Consisting of more than 300 articles written by ca 200 leading experts, this authoritative reference encompasses the entire fields of Geomagnetism and Paleomagnetism in a single volume. It describes in fine detail at an assessable level the state of the current knowledge and provides an up-to-date synthesis of the most basic concepts. As such, it will be an indispensable working tool not only for geophysicists and geophysics students but also for geologists, physicists, atmospheric and environmental scientists, and engineers.
Please note that this publication is available as print only OR online only OR print + online set. Save 75% of the online list price when purchasing the bundle. For more information on the online version please type the publication title into the search box above, then click on the "eReference" version in the results list.
The magnetic record left in rocks is studied in Paleomagnetism. Both fields have applications, pure and applied: in navigation, in the search for minerals and hydrocarbons, in dating rock sequences, and in unraveling past geologic movements such as plate motions they have contributed to a better understanding of the Earth.
Consisting of more than 300 articles written by ca 200 leading experts, this authoritative reference encompasses the entire fields of Geomagnetism and Paleomagnetism in a single volume. It describes in fine detail at an assessable level the state of the current knowledge and provides an up-to-date synthesis of the most basic concepts. As such, it will be an indispensable working tool not only for geophysicists and geophysics students but also for geologists, physicists, atmospheric and environmental scientists, and engineers.
Please note that this publication is available as print only OR online only OR print + online set. Save 75% of the online list price when purchasing the bundle. For more information on the online version please type the publication title into the search box above, then click on the "eReference" version in the results list.
Inhaltsverzeichnis zu „Encyclopedia of Geomagnetism and Paleomagnetism “
- Absolute Paleointensity Determinations Using Single Plagioclase Crystals- Adiabatic Gradient in the Core
- Aeromagnetic Surveying
- Agricola, Georgius
- Alfven H
- Alfven Waves
- Alfven's Theorem and the Frozen Flux approximation
- Ambient temperature and depth of burial of present erosion surface from remanent magnetization in dyke contact zones
- Anhysteretic Remanent Magnetization (ARM)
- Anisotropy of Magnetic Remanence
- Anisotropy of Magnetic Susceptibility
- Anisotropy of Magnetic Susceptibility and Rock Fabric: A historical Perspective
- Anisotropy of Magnetic Susceptibility Parameters
- Anti-dynamo and bounding theorems
- Archaeology, magnetic methods
- Archaeomagnetism
- Archeomagnetism
- Auroral Oval
- Baked Contact Test
- Bangui anomaly
- Barlow, P
- Bartels J
- Bauer L. A
- Bemmelen, W. van
- Benton E. R.
- Biomagnetism
- Boundary layers in the core
- Boussinesq and anelastic approximations
- Bullard E. C
- Carnegie, Reseach Vessel
- Champ
- Changes in magnetic mineralogy due to heating and methodological implications
- Chapman S
- Chemical Remanent Magnetism (CRM)
- Coast effect of induced currents
- Compass
- Conductivity Geothermometer
- Conductivity, ocean floor measurements
- Controlled source EM
- Convection, chemical
- Core Composition
- Core Convection
- Core Dynamics: instabilities
- Core Motions
- Core properties
- Physical
- Core properties
- theoretical determination
- Core-based inversions
- Core-mantle boundary topography: implications for dynamics
- Core-mantle boundary topography: seismology
- Core-mantle coupling, thermal
- Core-mantle coupling-electromagnetic
- Core-mantle coupling-topographic
- Cowling, T.G
- Cowling's Theorem
- Cox, Allen V. (Biography)
- Crustal Magnetic Field
- D" as a boundary layer
- D", anisotropy
- D", seismic properties
-
... mehr
D", composition
- Deciphering the Archives of Geomagnetic Reversals
- Della Porta, Giambattista
- Demagnetization
- Density distribution in the core
- Department of Terrestrial Magnetism, Carnegie Institution of Washington
- Depositional Remanent Magnetization (DRM)
- Depth to Curie temperature
- Dimensional analysis and time scales for the geodynamo
- Dipole moment variation
- Dynamo waves
- Dynamo, Backus
- Dynamo, Braginsky
- Dynamo, Bullard-Gellman
- Dynamo, Disk
- Dynamo, Gailitis
- Dynamo, Herzenberg
- Dynamo, Lowes-Wilkinson
- Dynamo, Model-Z
- Dynamo, Ponomarenko
- Dynamos, experimental
- Dynamos, fast
- Dynamos, Kinematic
- Dynamos, mean field
- Dynamos, Periodic
- Earth Structure, major divisions
- Effects of Heating on Anisotropy of Magnetic Susceptibility of Rocks
- Electrical anisotropy
- Electrical conductivity of the core
- Electrical conductivity of the mantle, mineralogy
- Electromagnetic ocean effects
- Ellipticity correction for the main field
- Elsasser W
- Energy source for the geodynamo
- Environmental Magnetism
- Environmental Magnetism: Paleomagnetic applications
- Equilibration of magnetic field: weak and strong field dynamos
- Euler Deconvolution
- Extraterrestrial Paleomagnetism
- First Order Reversal Curves
- Fisher Statistics as used in Paleomagnetic Research
- Fleming, JA
- Fluid dynamic experiments
- Fold Test; Analysis of Pre-Syn and Post folding Remanent Magnetization
- Forward Modelling of EM
- Galvanic Distortion
- Gauss C. F
- Gauss' determination of absolute intensity
- Gellibrand H
- Geocentric Axial Dipole Hypothesis
- Geodynamo
- Geodynamo: Numerical simulations
- Geomagnetic Deep Sounding
- Geomagnetic Dipole Field
- Geomagnetic Excursions
- Geomagnetic Field: Asymmetries
- Geomagnetic Hazards
- Geomagnetic Jerks
- Geomagnetic Polarity Time Scale
- Geomagnetic pulsations
- Geomagnetic Reversal Sequence: Statistical Structure
- Geomagnetic Secular Variation
- Geomagnetic Spatial Spectrum
- Geomagnetic temporal spectrum
- Gilbert W
- Gravitational torque
- Gravity-inertio waves and inertial oscillations
- Gruneisen's parameter for iron and Earth's core
- Halley, E
- Hansteen, C
- Hartmann, Georg
- Heat flow across the core-mantle boundary
- Helioseismology
- Higgins-Kennedy Paradox
- History of Geomagnetism
- History of Instrumentation
- Humboldt, A.v. and Magnetic storms
- Humbolt A. v
- Hysteresis Measurements in Rock Magnetism
- IAGA
- Ideal solution theory
- IGRF
- International Geomagnetic Reference Field
- Induction arrows
- Induction from satellite data
- Industrial uses of EM
- Inhomogeneous boundary conditions and the dynamo
- Inner core anisotropy
- Inner core composition
- Inner core oscillation
- Inner core rotation
- Inner core rotational dynamics
- Inner core tangent cylinder
- Inner core: PKJKP
- Interiors of Planets and Satellites
- Internal external field separation
- Inverse modelling of EM
- Ionosphere
- Iron Sulphides
- Isothermal Remanent Magnetization (IRM)
- Jesuits, role in Geomagnetism
- Key Paleomagnetic Pole
- Kircher, A
- Lake bottom EM measurements
- Land uses of EM
- Langel R.A
- Larmor J
- Lehmann, I
- Length of day variations
- decadal
- Length of day variations
- long term
- Lloyd, H
- Low Temperature Rock Magnetism
- Low-Field Magnetic Susceptibility (MS) of Sediments and Sedimentary Rocks
- Magnetic Anisotropy of Sedimentary Rocks and Strain Alteration
- Magnetic anomalies for geology and resources
- Magnetic anomalies, long wavelength
- Magnetic Domains
- Magnetic Field of Mars
- Magnetic Proxy Parameters
- Magnetic Susceptibility
- Magnetic Susceptibility of Solids
- Magnetization of the Oceanic Crust
- Magnetoconvection
- Magnetohydrodynamic waves
- Magnetohydrodynamics
- Magnetometers
- Magnetosphere of the Earth
- Magnetostatic Shielding
- Magnetostratigraphy
- Magnetotellurics
- Magsat
- Main field maps
- Main Field Modelling
- Marine controlled source electromagnetics
- Marine magnetic anomalies
- Marine magnetic surveys
- Matuyama, M. (Biography)
- Maynard Blackett of Chelsea, Patrick (Biography)
- Melting temperature of iron in the core, experimental
- Melting temperature of iron in the core, theory
- Microwave and Shaw Absolute Paleointensity Techniques
- Model of Secular Variation of the Earth's Magnetic Field 6899 words
- Modelling magnetic anomalies
- Nagata, Takesi (Biography)
- Natural Remanent Magnetization (NRM)
- Natural sources for electromagnetic induction studies
- Neel, Louis (Biography)
- Non-dipole field
- Non-dynamo theories
- Norman R
- Observatories 01
- an overview
- Observatories 02
- Observatory Instrumentation
- Observatories 03
- Observatory automation
- Observatories 04
- Intermagnet
- Observatories 05
- Observatory programme in Australia
- Observatories 06
- Observatory programme in the British Isles
- Observatories 07
- Observatory programme in France
- Observatories 08
- Observatory programme in USA
- Observatories 09
- Observatories in Antarctica
- Observatories 10
- Observatories in Benelux countries
- Observatories 11
- Observatories in Canada
- Observatories 12
- Observatories in China
- Observatories 13
- Observatories in East and Central Europe
- Observatories 14
- Observatories in Germany
- Observatories 15
- Observatories in India
- Observatories 16
- Observatories in Italy
- Observatories 17
- Observatories in Japan and Asia
- Observatories 18
- Observatories in Latin American
- Observatories 19
- Observatories in New Zealand and the South Pacific
- Observatories 20
- Observatories in Nordic countries
- Observatories 21
- Observatories in Russia
- Observatories 22
- Observatories in southern Africa
- Observatories 23
- Observatories in Spain
- Oersted
- Oldham, RD
- Origin of the Core
- Pacific Dipole Window
- Paleomagnetic field collection Methods
- Paleomagnetic records of the last polarity transition and the process of field reversals
- Paleomagnetic Secular Variation
- Paleomagnetism
- Paleomagnetism: Deep-Sea Sediments
- Paleomagnetism: Orogenic Belts
- Paleosecular variation: Models and Statistics
- Parkinson D
- Periodic external fields
- Petrus Peregrinus
- Piezo-remanent magnetization
- Planetary and Satellite dynamos
- Plate Tectonics of China
- POGO (OGO-2,
- 4 and
- 6 spacecraft)
- Polarity Reversals
- Potential vorticity and potential magnetic field theorems
- Precession and core dynamics
- Price, A
- Principal Component Analyses
- Principal Component Analysis and Bingham Distribution
- Project MAGNET
- Proudman-Taylor theorem
- Radioactive isotopes, their decay in mantle and core
- Radioisotopic Dating of Polarity Transitions and Excursions of the Earth's Magnetic Field Recorded in Lava
- Reduction to pole
- Regional studies of EM
- Relative Absolute Paleointensity of Sediments
- Repeat stations
- Reversal Transition Fields
- Reversals, theory
- Rikitake, T
- Ring Current
- Robust electromagnetic transfer functions estimates
- Rock Magnetism
- Rotating convection, non-magnetic
- Runcorn, S. Keith (Biography)
- Runcorn's theorem
- Sabine E
- Seamount magnetism
- SEDI
- Seismic phases
- Seismic velocities of inner core
- Seismo-electromagnetic effects
- Shock wave experiments
- Solar Dynamo
- Spherical Cap Harmonics
- Spherical harmonics
- Spinner Magnetometers
- Statistical methods for paleomagnetic data
- Storms and substorms
- Sun's Magnetic Field
- Superchrons and Changes in Reversal Frequency
- Superconducting Rock Magnetometers
- Symmetry and the geodynamo
- Taylor's condition
- Techniques for absolute paleointensity
- Tectonic interpretation of EM
- Temperature of the Earth's core
- Thellier, Emile (Biography)
- Thermal conduction in the core
- Thermal conductivity of the mantle
- Thermal wind
- Thermoremanent Magnetization (TRM)
- Thermoremanent Magnetization in magnetic minerals from experiment and Theory
- Time-dependent models of the main magnetic field
- Torsional oscillations
- Transfer functions
- Transient electromagnetic induction
- True Polar Wander
- Turbulence in the Earth's core
- ULVZ's
- Uniqueness of solutions to Laplace's equation
- Units
- Upward and Downward continuation
- Variable Field Translation Balance
- Verhoogen J
- Vine-Matthews-Morley hypothesis
- Viscosity of the core
- Viscous Remanent Magnetization (VRM) And Viscous Remagnetization
- Volcano-electromagnetic effects
- Voyages making geomagnetic measurements
- Watkins, Norman (Biography)
- Westward drift.
- Deciphering the Archives of Geomagnetic Reversals
- Della Porta, Giambattista
- Demagnetization
- Density distribution in the core
- Department of Terrestrial Magnetism, Carnegie Institution of Washington
- Depositional Remanent Magnetization (DRM)
- Depth to Curie temperature
- Dimensional analysis and time scales for the geodynamo
- Dipole moment variation
- Dynamo waves
- Dynamo, Backus
- Dynamo, Braginsky
- Dynamo, Bullard-Gellman
- Dynamo, Disk
- Dynamo, Gailitis
- Dynamo, Herzenberg
- Dynamo, Lowes-Wilkinson
- Dynamo, Model-Z
- Dynamo, Ponomarenko
- Dynamos, experimental
- Dynamos, fast
- Dynamos, Kinematic
- Dynamos, mean field
- Dynamos, Periodic
- Earth Structure, major divisions
- Effects of Heating on Anisotropy of Magnetic Susceptibility of Rocks
- Electrical anisotropy
- Electrical conductivity of the core
- Electrical conductivity of the mantle, mineralogy
- Electromagnetic ocean effects
- Ellipticity correction for the main field
- Elsasser W
- Energy source for the geodynamo
- Environmental Magnetism
- Environmental Magnetism: Paleomagnetic applications
- Equilibration of magnetic field: weak and strong field dynamos
- Euler Deconvolution
- Extraterrestrial Paleomagnetism
- First Order Reversal Curves
- Fisher Statistics as used in Paleomagnetic Research
- Fleming, JA
- Fluid dynamic experiments
- Fold Test; Analysis of Pre-Syn and Post folding Remanent Magnetization
- Forward Modelling of EM
- Galvanic Distortion
- Gauss C. F
- Gauss' determination of absolute intensity
- Gellibrand H
- Geocentric Axial Dipole Hypothesis
- Geodynamo
- Geodynamo: Numerical simulations
- Geomagnetic Deep Sounding
- Geomagnetic Dipole Field
- Geomagnetic Excursions
- Geomagnetic Field: Asymmetries
- Geomagnetic Hazards
- Geomagnetic Jerks
- Geomagnetic Polarity Time Scale
- Geomagnetic pulsations
- Geomagnetic Reversal Sequence: Statistical Structure
- Geomagnetic Secular Variation
- Geomagnetic Spatial Spectrum
- Geomagnetic temporal spectrum
- Gilbert W
- Gravitational torque
- Gravity-inertio waves and inertial oscillations
- Gruneisen's parameter for iron and Earth's core
- Halley, E
- Hansteen, C
- Hartmann, Georg
- Heat flow across the core-mantle boundary
- Helioseismology
- Higgins-Kennedy Paradox
- History of Geomagnetism
- History of Instrumentation
- Humboldt, A.v. and Magnetic storms
- Humbolt A. v
- Hysteresis Measurements in Rock Magnetism
- IAGA
- Ideal solution theory
- IGRF
- International Geomagnetic Reference Field
- Induction arrows
- Induction from satellite data
- Industrial uses of EM
- Inhomogeneous boundary conditions and the dynamo
- Inner core anisotropy
- Inner core composition
- Inner core oscillation
- Inner core rotation
- Inner core rotational dynamics
- Inner core tangent cylinder
- Inner core: PKJKP
- Interiors of Planets and Satellites
- Internal external field separation
- Inverse modelling of EM
- Ionosphere
- Iron Sulphides
- Isothermal Remanent Magnetization (IRM)
- Jesuits, role in Geomagnetism
- Key Paleomagnetic Pole
- Kircher, A
- Lake bottom EM measurements
- Land uses of EM
- Langel R.A
- Larmor J
- Lehmann, I
- Length of day variations
- decadal
- Length of day variations
- long term
- Lloyd, H
- Low Temperature Rock Magnetism
- Low-Field Magnetic Susceptibility (MS) of Sediments and Sedimentary Rocks
- Magnetic Anisotropy of Sedimentary Rocks and Strain Alteration
- Magnetic anomalies for geology and resources
- Magnetic anomalies, long wavelength
- Magnetic Domains
- Magnetic Field of Mars
- Magnetic Proxy Parameters
- Magnetic Susceptibility
- Magnetic Susceptibility of Solids
- Magnetization of the Oceanic Crust
- Magnetoconvection
- Magnetohydrodynamic waves
- Magnetohydrodynamics
- Magnetometers
- Magnetosphere of the Earth
- Magnetostatic Shielding
- Magnetostratigraphy
- Magnetotellurics
- Magsat
- Main field maps
- Main Field Modelling
- Marine controlled source electromagnetics
- Marine magnetic anomalies
- Marine magnetic surveys
- Matuyama, M. (Biography)
- Maynard Blackett of Chelsea, Patrick (Biography)
- Melting temperature of iron in the core, experimental
- Melting temperature of iron in the core, theory
- Microwave and Shaw Absolute Paleointensity Techniques
- Model of Secular Variation of the Earth's Magnetic Field 6899 words
- Modelling magnetic anomalies
- Nagata, Takesi (Biography)
- Natural Remanent Magnetization (NRM)
- Natural sources for electromagnetic induction studies
- Neel, Louis (Biography)
- Non-dipole field
- Non-dynamo theories
- Norman R
- Observatories 01
- an overview
- Observatories 02
- Observatory Instrumentation
- Observatories 03
- Observatory automation
- Observatories 04
- Intermagnet
- Observatories 05
- Observatory programme in Australia
- Observatories 06
- Observatory programme in the British Isles
- Observatories 07
- Observatory programme in France
- Observatories 08
- Observatory programme in USA
- Observatories 09
- Observatories in Antarctica
- Observatories 10
- Observatories in Benelux countries
- Observatories 11
- Observatories in Canada
- Observatories 12
- Observatories in China
- Observatories 13
- Observatories in East and Central Europe
- Observatories 14
- Observatories in Germany
- Observatories 15
- Observatories in India
- Observatories 16
- Observatories in Italy
- Observatories 17
- Observatories in Japan and Asia
- Observatories 18
- Observatories in Latin American
- Observatories 19
- Observatories in New Zealand and the South Pacific
- Observatories 20
- Observatories in Nordic countries
- Observatories 21
- Observatories in Russia
- Observatories 22
- Observatories in southern Africa
- Observatories 23
- Observatories in Spain
- Oersted
- Oldham, RD
- Origin of the Core
- Pacific Dipole Window
- Paleomagnetic field collection Methods
- Paleomagnetic records of the last polarity transition and the process of field reversals
- Paleomagnetic Secular Variation
- Paleomagnetism
- Paleomagnetism: Deep-Sea Sediments
- Paleomagnetism: Orogenic Belts
- Paleosecular variation: Models and Statistics
- Parkinson D
- Periodic external fields
- Petrus Peregrinus
- Piezo-remanent magnetization
- Planetary and Satellite dynamos
- Plate Tectonics of China
- POGO (OGO-2,
- 4 and
- 6 spacecraft)
- Polarity Reversals
- Potential vorticity and potential magnetic field theorems
- Precession and core dynamics
- Price, A
- Principal Component Analyses
- Principal Component Analysis and Bingham Distribution
- Project MAGNET
- Proudman-Taylor theorem
- Radioactive isotopes, their decay in mantle and core
- Radioisotopic Dating of Polarity Transitions and Excursions of the Earth's Magnetic Field Recorded in Lava
- Reduction to pole
- Regional studies of EM
- Relative Absolute Paleointensity of Sediments
- Repeat stations
- Reversal Transition Fields
- Reversals, theory
- Rikitake, T
- Ring Current
- Robust electromagnetic transfer functions estimates
- Rock Magnetism
- Rotating convection, non-magnetic
- Runcorn, S. Keith (Biography)
- Runcorn's theorem
- Sabine E
- Seamount magnetism
- SEDI
- Seismic phases
- Seismic velocities of inner core
- Seismo-electromagnetic effects
- Shock wave experiments
- Solar Dynamo
- Spherical Cap Harmonics
- Spherical harmonics
- Spinner Magnetometers
- Statistical methods for paleomagnetic data
- Storms and substorms
- Sun's Magnetic Field
- Superchrons and Changes in Reversal Frequency
- Superconducting Rock Magnetometers
- Symmetry and the geodynamo
- Taylor's condition
- Techniques for absolute paleointensity
- Tectonic interpretation of EM
- Temperature of the Earth's core
- Thellier, Emile (Biography)
- Thermal conduction in the core
- Thermal conductivity of the mantle
- Thermal wind
- Thermoremanent Magnetization (TRM)
- Thermoremanent Magnetization in magnetic minerals from experiment and Theory
- Time-dependent models of the main magnetic field
- Torsional oscillations
- Transfer functions
- Transient electromagnetic induction
- True Polar Wander
- Turbulence in the Earth's core
- ULVZ's
- Uniqueness of solutions to Laplace's equation
- Units
- Upward and Downward continuation
- Variable Field Translation Balance
- Verhoogen J
- Vine-Matthews-Morley hypothesis
- Viscosity of the core
- Viscous Remanent Magnetization (VRM) And Viscous Remagnetization
- Volcano-electromagnetic effects
- Voyages making geomagnetic measurements
- Watkins, Norman (Biography)
- Westward drift.
... weniger
Autoren-Porträt
David Gubbins is Research Professor of Earth Sciences in the School of Earth & Environment, University of Leeds, UK. He did his PhD on geomagnetic dynamos in Cambridge, supervised by Sir Edward Bullard (qv.) and has worked in the USA and in Cambridge before moving to Leeds in 1989. His work has included dynamo theory and its connection with the Earth's thermal history, modelling the Earth's magnetic field from historical measurements, and recently the interpretation of paleomagnetic data. He is a Fellow of the Royal Society and has been awarded the Gold Medal of the Royal Astronomical Society and the John Adam Fleming (qv.) Medal of the American Geophysical Union for original research and leadership in geomagnetism.Emilio Herrero-Bervera is Research Professor of Geophysics at the School of Ocean Earth Science and Technology (SOEST) within the Hawaii Institute of Geophysics and Planetology (HIGP) of the University of Hawaii at Manoa, where he is the head of the Paleomagnetics and Petrofabrics Laboratory. During his career he has published over 90 papers in professional journals including Nature, JGR, EPSL, JVGR. He has worked in such diverse fields as volcanology, sedimentology, plate tectonics and has done field work on 5 continents
Bibliographische Angaben
- 2007, 1054 Seiten, mit farbigen Abbildungen, Maße: 28 cm, Gebunden, Englisch
- Herausgegeben:Gubbins, David; Herrero-Bervera, Emilio
- Verlag: Springer Netherlands
- ISBN-10: 1402039921
- ISBN-13: 9781402039928
Sprache:
Englisch
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