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Books > Academic & Education > Professional & Technical > Geophysics
This book is a collection of 22 selected papers from the homonymous Conference held in September 2003 Milos, Greece. The aim of the conference was to serve as a forum for the presentation and constructive discussion of the state-of-the-art and emerging issues on the South Aegean Volcanic Arc.
This volume covers the formation and biogeochemistry of a variety of important sediment types from their initial formation through their conversion (diagenesis) to sedimentary rocks. The volume deals with the chemical, mineralogical, and isotopic properties of sediments and sedimentary rocks and their use in interpreting the environment of formation and subsequent events in the history of sediments, and the nature of the ocean-atmosphere system through geological time.
This book is a continuation of 'Acoustic and Elastic Wave Fields in
Geophysics, Part I' published in 2000. The second volume is
dedicated to propagation of linear plane, spherical and cylindrical
acoustic waves in different media. Chapter 1 is devoted to
principles of geometric acoustic in plane wave approximation. The
eikonal and transport equations are derived. Ray tracing and
wavefront construction techniques are explained. Chapter 2 deals
with dynamic properties of wave fields. The behavior of pressure
and displacements amplitudes in zero approximation is analysed in
two ways: using Poynting vector and solving the transport equation.
This chapter contains several examples related to shadow zones and
caustics. In Chapter 3 using the results of analysis of
high-frequency wave kinematics and dynamics some fundamental
aspects of Kirchhoff migration are described. Chapters 4 and 5 are
devoted to propagation of plane waves in media with flat boundaries
in the case of normal and oblique incidence. Special attention is
paid to the case when an incident angle exceeds the critical
angles. Formation of normal modes in the waveguide is discussed.
Chapter 6 deals with a spherical wave reflection and refraction.
The steepest descent method is introduced to describe the behavior
of reflected, transmitted, head and evanescent waves. In Chapter 7
propagation of stationary and transient waves in a waveguide formed
by a flat layer with low velocity are investigated. Normal modes
and waves related to the branch points of integrands under
consideration are studied. Dispersive properties of normal modes
are discussed. Chapter 8 describes wave propagation inside cylinder
in acoustic media. Several appendices are added to help the reader
understand different aspects of mathematics used in the book.
"Geosciences, Environment and Man" has three major objectives, which determine the division in three parts of this volume: I. To consider the main natural geological processes interfering with and therefore threatening the activities of man: earthquakes, volcanic eruptions, land movements, floods, wind and coastal risks; main prevention and mitigation measures against these natural hazards are presented. II. To examine the exploitation of earth's natural resources such as materials, ores and minerals, fossil fuels, water, radioactivity, and the resulting consequences on solid Earth balance and future. III. To assess the hold level reached by the activities of man on planet surface envelopes through agriculture, urbanization, industrialization, and communication; the local to global effects of human influence triggered by recent demographic growth on underground, soils, water and air characters are taken into account. Both deteriorating and beneficial aspects of Earth - the interactions of man are emphasized, as well as mitigation or restoration measures and perspectives.
This book examines different classical and modern aspects of geophysical data processing and inversion with emphasis on the processing of seismic records in applied seismology.
The nature of global change in the Pacific Basin is poorly known
compared to other parts of the world. Climate, Environment, and
Society in the Pacific during the Last Millennium describes the
climate changes that occurred in the Pacific during the last
millennium and discusses how these changes controlled the broad
evolution of human societies, typically filtered by the effects of
changing sea level and storminess on food availability and
interaction. Covering the entire period since AD 750 in the
Pacific, this book describes the influences of climate change on
environments and societies during the Medieval Warm Period and the
Little Ice Age, focusing on the 100-year transition between these -
a period of rapid change known as the AD 1300 Event.
Adsorption of Metals by Geomedia II serves as a needed resource for
this topic which has received much attention during the past 25
years. The book provides an in-depth review of the field, followed
by numerous chapters that document the current status of adsorption
research for a variety of metals by geomedia ranging from
individual minerals to sediments and soils. Adsorption mechanisms
are detailed and precipitation is presented as a distinct sorption
process. Virtually all factors affecting the extent of metal
adsorption are examined, including the effects of selected anions,
competition among metals, pH, metal concentration, loading,
variable metal adsorption capacity, ionic strength, hydrogen
exchange and stoichiometry, and solids concentration. A variety of
adsorption models are briefly presented and some are used to extend
laboratory studies to field sites.
The history of Earth in the Solar System has been unraveled using natural radioactivity. The sources of this radioactivity are the original creation of the elements and the subsequent bombardment of objects, including Earth, in the Solar System by cosmic rays. Both radioactive and radiogenic nuclides are harnessed to arrive at ages of various events and processes on Earth. This collection of chapters from the Treatise on Geochemistry
displays the range of radioactive geochronometric studies that have
been addressed by researchers in various fields of Earth science.
These range from the age of Earth and the Solar System to the
dating of the history of Earth that assists us in defining the
major events in Earth history. In addition, the use of radioactive
geochronometry in describing rates of Earth surface processes,
including the climate history recorded in ocean sediments and the
patterns of circulation of the fluid Earth, has extended the range
of utility of radioactive isotopes as chronometric and tracer
tools.
Geochemistry of Earth Surface Systemsoffers an interdisciplinary
reference for scientists, researchers and upper undergraduate and
graduate levelgeochemistry students a sampling of articles on earth
surface processes from The Treatise on Geochemistry that ismore
affordable than the full Treatise. For professionals, this volume
will provide anoverview of the field as a whole. For students, it
will provide morein-depth introductory content thanis found
inbroad-based geochemistry textbooks. Articleswere selected from
chapters across all volumes of the full Treatise, and include:
Volcanic Degassing, Hydrothermal Processes, The Contemporary Carbon
Cycle, Global Occurrence of Major Elements in Rivers, Organic
Matter in the Contemporary Ocean, The Biological Pump, and
Evolution of Sedimentary Rocks.
The book deals with the record of important Neoproterozoic to Early
Palaeozoic events in southwestern Gondwana, that heralded the
Cambrian explosion and the dawn of modern ecosystems. It contains a
detailed account of the Neoproterozoic to Cambrian geological
record in a poorly-known part of the world, which is at the same
time key to understand fundamental processes at the
Proterozoic-Cambrian transition. The emphasis is placed on litho-,
bio-, chemostratigraphy and magmatism. The palaeoclimatic,
tectonic, evolutionary radiation and extinction events and
associated mineralizations will be identified and discussed. A
synthesis of all data is provided at the end of the book,
integrating the data from all cratons and fold belts in
southwestern Gondwana. The events will be individualized, their
impact discussed and correlations between different successions
both within and outside Gondwana proposed.
Treatise on Geophysics: Mantle Dynamics, Volume 7 aims to provide both a classical and state-of-the-art introduction to the methods and science of mantle dynamics, as well as survey leading order problems (both solved and unsolved) and current understanding of how the mantle works. It is organized around two themes: (1) how is mantle convection studied; and (2) what do we understand about mantle dynamics to date. The first four chapters are thus concerned with pedagogical reviews of the physics of mantle convection; laboratory studies of the fluid dynamics of convection relevant to the mantle; theoretical analysis of mantle dynamics; and numerical analysis and methods of mantle convection. The subsequent chapters concentrate on leading issues of mantle convection itself, which include the energy budget of the mantle; the upper mantle and lithosphere in and near the spreading center (mid-ocean ridge) environment; the dynamics of subducting slabs; hot spots, melting anomalies, and mantle plumes; and finally, geochemical mantle dynamics and mixing.
Treaties on Geophysics: Core Dynamics, Volume 8, provides a comprehensive review of the current state of understanding of core dynamics. The book begins by analyzing a subject of long-standing and on-going controversy: the gross energetics of the core. It then explains the important elements of dynamo theory; actual fluid motions in the core; the basic physical principles involved in thermochemical convection in the core and the basic equations governing the convection; and turbulence and the small-scale dynamics of the core. This is followed by discussions of the state of knowledge on rotation-induced core flows; the use of first-principles numerical models of self-sustaining fluid dynamos; and the behavior of polarity reversals in numerical dynamo models. The remaining chapters cover the various roles the inner core plays in core dynamics and the geodynamo; experiments that have shaped knowledge about the flows in the core that produce the geodynamo and govern its evolution; and ways the mantle can affect core dynamics, and corresponding ways the core can affect the mantle.
Geodesy, which is the science of measuring the size and shape of the Earth, explores the theory, instrumentation and results from modern geodetic systems. The beginning sections of the volume cover the theory of the Earth's gravity field, the instrumentation for measuring the field, and its temporal variations. The measurements and results obtained from variations in the rotation of the Earth are covered in the sections on short and long period rotation hanges. Space based geodetic methods, including the global positioning system (GPS) and Interferometric synthetic aperture radar (SAR), are also examined in detail. Self-contained volume starts with an overview of the subject
then explores each topic with in depth detail
Treatise on Geophysics: Geomagnetism, Volume 5, provides an overview of the most important aspects of geomagnetism. The book begins by tracing the history of the study of geomagnetism. It then reviews global models of the Earth's magnetic field; the main sources of external magnetic field contributions; and the instruments and practices used to observe and measure the full range of features of the geomagnetic field. It discusses the origins of current knowledge of the secular variation of the Earth's magnetic field; crustal magnetism; geomagnetic excursions; the study of geophysical electromagnetic induction; the magnetization process; and the status of recent magnetic field data and their applications. The remaining chapters cover the geometry of the geomagnetic field and its temporal variability as recorded in volcanic and sedimentary rocks over the past few million years; the ocean crust as a recorder of geomagnetic field variations; and the theoretical basis for paleointensity experiments in igneous and sedimentary environments. The final chapter explains the concept of true polar wander (TPW), defined as shifts in the geographic location of Earth's daily rotation axis and/or by fluctuations in the spin rate (length of day anomalies).
Evolution of the Earth focuses on the formation of Earth. Topics
include the differention of the core, mantle and crust; the
formation of the ocean basins and continents; outgassing and
volcanism; the initiation of plate tectonics, the origin and
persistence of Earth's magnetic field; the growth of the inner
core; changes in mantle convection through time; and the impact of
life on the planet. The volume takes an interdisciplinary viewpoint
that emphasizes the interplay of geophysics, other aspects of earth
science and biological evolution. Some outstanding questions are
identified and debated.
Treatise on Geophysics: Mineral Physics, Volume 2, provides a comprehensive review of the current state of understanding of mineral physics. Each chapter demonstrates the significant progress that has been made in the understanding of the physics and chemistry of minerals, and also highlights a number of issues which are still outstanding or that need further work to resolve current contradictions. The book first reviews the current status of our understanding of the nature of the deep Earth. These include the seismic properties of rocks and minerals; problems of the lower mantle and the core-mantle boundary; and the state of knowledge on mantle chemistry and the nature and evolution of the core. The discussions then turn to the theory underlying high-pressure, high-temperature physics, and the major experimental methods being developed to probe this parameter space. The remaining chapters explain the specific techniques for measuring elastic and acoustic properties, electronic and magnetic properties, and rheological properties; the nature and origin of anisotropy in the Earth; the properties of melt; and the magnetic and electrical properties of mantle phases.
Ground-penetrating radar (GPR) is a rapidly developing field that
has seen tremendous progress over the past 15 years. The
development of GPR spans aspects of geophysical science,
technology, and a wide range of scientific and engineering
applications. It is the breadth of applications that has made GPR
such a valuable tool in the geophysical consulting and geotechnical
engineering industries, has lead to its rapid development, and
inspired new areas of research in academia. The topic of GPR has
gone from not even being mentioned in geophysical texts ten years
ago to being the focus of hundreds of research papers and special
issues of journals dedicated to the topic. The explosion of primary
literature devoted to GPR technology, theory and applications, has
lead to a strong demand for an up-to-date synthesis and overview of
this rapidly developing field. Because there are specifics in the
utilization of GPR for different applications, a review of the
current state of development of the applications along with the
fundamental theory is required. This book will provide sufficient
detail to allow both practitioners and newcomers to the area of GPR
to use it as a handbook and primary research reference.
This book serves as an up-to-date introduction, as well as overview
to modern trace fossil research and covers nearly all of the
essential aspects of modern ichnology. Divided into three section,
Trace Fossils covers the historical background and concepts of
ichnology, on-going research problems, and indications about the
possible future growth of the discipline and potential connections
to other fields. This work is intended for a broad audience of
geological and biological scientists. Workers new to the field
could get a sense of the main concepts of ichnology and a clear
idea of how trace fossil research is conducted. Scientists in
related disciplines could find potential uses for trace fossils in
their fields. And, established workers could use the book to check
on the progress of their particular brand of ichnology. By design,
there is something here for novice and veteran, insider and
outsider, and for the biologically-oriented workers and for the
sedimentary geologists.
Based on lectures given in the First Russian School-Seminar on
electromagnetic soundings of the Earth held in Moscow on 15th
November, 2003, this book acquaints scientists and technologists
with the latest achievements in theory, techniques and practical
applications of the methods of electromagnetic sounding. This three
part text covers the methods considered for Earth electromagnetic
sounding on a global, regional, and local scale; modern methods for
solving forward and inverse problems of geoelectrics, particularily
contemporary approaches to the EM data modeling and interpretation
in the class of three-dimensional models; and the results of
regional EM on-land and sea soundings
Principles of Sequence Stratigraphy provides an in-depth coverage and impartial assessment of all current ideas and models in the field of sequence stratigraphy. Even though widely popular among all groups interested in the analysis of sedimentary basin fills, both in academia and in the industry, sequence stratigraphy is yet a difficult undertaking due to an overwhelming jargon and the persistence of conflicting approaches as to how the sequence stratigraphic method should be applied to the rock record. This textbook examines the relationship between such conflicting approaches from the perspective of a unifying platform, demonstrating that sufficient common ground exists to eliminate terminology barriers and to facilitate communication between all practitioners of sequence stratigraphy.
The book deals with the study of three important volcanisms in the Campania Plain: Vesuvius, Campi Flegrei and Ignimbrites. The knowledge of the volcanic evolution of Vesuvius and Campi Flegrei has a particular relevance because of the hazards that these volcanoes pose to the about 1.5 million people living in the Neapolitan area.
The oceans are vitally important to an understanding of how the Earth works as an integrated system because its chemical composition records transfer of elements through the Earth's geochemical reservoirs as well as defining how physical, biological and chemical processes combine to influence issues as diverse as climate change and the capacity of the oceans to remove toxic metals. Much modern marine geochemistry aims to link and integrate studies of the modern oceans with work using proxies to define how ocean chemistry and the ocean/atmospheric system has changed through time on a number of different timescales. Special focus in such work is the carbon cycle and its link to changes in greenhouse gases in the atmosphere. Volume 6 covers all the important topics needed for such an integrated approach, ranging from the contemporary ocean composition, transport processes in the ocean, paleoclimatology and paleo-oceanography from marine deposits, to the evolution of seawater composition.
Volume 3 examines the chemical composition of the Earth's crust, starting with the continental crust and the rocks exposed therein, moving on to oceanic crust (MORB and oceanic plateaus) and finishing with island arc crust. In addition to providing a descriptive geochemistry of the Earth's crust, the volume summarizes the processes responsible for crustal formation and modification, exchange between the crust and other Earth reservoirs (mantle, oceans and atmosphere), and examines the secular evolution of the crust.
High-pressure mineral physics is a field that is strongly driven by the development of new technology. Fifty years ago, when experimentally achievable pressures were limited to just 25 GPa, little was know about the mineralogy of the Earth's lower mantle. Silicate perovskite, the likely dominant mineral of the deep Earth, was identified only when the high-pressure techniques broke the pressure barrier of 25 GPa in 1970s. However, as the maximum achievable pressure reached beyond one Megabar (100 GPa) and even to the pressure of Earth's core on minute samples, new discoveries increasingly were fostered by the development of new analytical techniques and improvements in sensitivity and precision of existing techniques.
This second volume of Frontiers articles contains a broad array of
fascinating topics. The first four |
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