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Author: David J. Dunlop Publisher: Cambridge University Press ISBN: 9780521000987 Category : Nature Languages : en Pages : 600
Book Description
This book is a comprehensive treatment of fine particle magnetism and the magnetic properties of rocks. Starting from atomic magnetism and magneotistic principles, the authors explain why domains and micromagnetic structures form in ferrmagnetic crystals and how these lead to magnetic memory in the form of thermal, chemical and other remanent magnetizations. This book will be of value to graduate students and researchers in geophysics and geology, particularly in palemagnetism and rock magnetism, as well as physicists and electrical engineers interested in fine-particle magnetism and magnetic recording.
Author: David J. Dunlop Publisher: Cambridge University Press ISBN: 9780521000987 Category : Nature Languages : en Pages : 600
Book Description
This book is a comprehensive treatment of fine particle magnetism and the magnetic properties of rocks. Starting from atomic magnetism and magneotistic principles, the authors explain why domains and micromagnetic structures form in ferrmagnetic crystals and how these lead to magnetic memory in the form of thermal, chemical and other remanent magnetizations. This book will be of value to graduate students and researchers in geophysics and geology, particularly in palemagnetism and rock magnetism, as well as physicists and electrical engineers interested in fine-particle magnetism and magnetic recording.
Author: Colin F. Williams Publisher: ISBN: Category : Argillite Languages : en Pages : 214
Book Description
Phosphatic concretions occur within diatomite in the upper part of the Miocene Monterey Formation near Lompoc, Calif. Absence of disruption of fine laminar bedding in the associated sediment by the concretions shows that they formed after complete compaction of the enclosing sediment.The concretions exhibit a strongly concentric color, chemical, and mineralogic zonation. Many of them are composed of a nucleus in which vivianite is the dominant mineral. Amorphous ferric phosphate, mitridatite, and francolite are the dominant phosphatic phases in successive layers toward the surface of the concretions. Cd and As contents increase tenfold from the nucleus outward, reaching a maximum of 2,000 ppm, whereas Ni content, with a maximum of 720 ppm, and Co content show the opposite trend. This mineralogy and elemental composition favor accretion under conditions of continuously increasing Eh and pH, during uplift into the fresh-ground-water zone of the terrestrial environment. Shale-normalized rare-earth-element patterns, however, suggest a marine source for the elements biogenic debris consisting of opal-A, organic matter, and carbonates of the enclosing sediment.
Author: Curtis E. Larsen Publisher: ISBN: Category : Algonquin, Lake Languages : en Pages : 302
Book Description
Quantitative and qualitative study of stream,-profile data is used to infer recency of uplift which grossly correlates with rates of seismicity.
Author: David J. Dunlop
Author: David J. Dunlop
Author: 
Author: Colin F. Williams
Author: Curtis E. Larsen
Author: E. A. Du Bray
Author: Henry W. Roehler
Author: Helaine W. Markewich
Author: Gilpin R. Robinson (Jr.)
Author: Donald Edward White
Author: Margo I. Toth