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Books > Academic & Education > Professional & Technical > Geophysics
In recognition of the fundamental control exerted by weathering on
landscape evolution and topographic development, the 35th
Binghamton Geomorphology Symposium was convened under the theme of
Weathering and Landscape Evolution. The papers and posters
presented at the conference imparted the state-of-the-art in
weathering geomorphology, tackled the issue of scale linkage in
geomorphic studies and offered a vehicle for interdisciplinary
communication on research into weathering and landscape evolution.
The papers included in this book are encapsulated here under the
general themes of weathering mantles, weathering and relative
dating, weathering and denudation, weathering processes and
controls and the 'big picture'.
Volume 9 focuses on natural and anthropogenic environmental contaminants and their implications for human health and the environment. Environmental impacts on soils, groundwater, freshwater, the oceans and atmosphere are examined in the context of both inorganic geochemistry (metals, metalloids, radioactive compounds, mineral dusts, dissolved salts, acidification) and organic geochemistry (halogenated and non-halogenated hydrocarbons, volatile organic compounds, fuel oxygenates, pesticides, nutrients). Issues of risk, toxicity and exposure assessment; contaminant fate and transport; remediation and disposal; and source identification are examined in this context.
Written by one of Korea's most respected earth scientists, "Geology and Sedimentology of the Korean Peninsula" analyzes sedimentary facies, basin evolution, and sequence stratigraphy to provide answers to depositional processes and environmental changes through the Earth's history, including tectonic events, climate changes, and sea-level fluctuations. This is one of the first books covering the geology of the Korean peninsula. It offers an in-depth exploration of this region, which also allows comparison with sedimentary basins around the world. This is an important book for students, researchers, and professionals working in the geography of East Asia. The study of sedimentary basins can help advance basic
understanding of how the Earth's crust developed, as well as offer
insights into the influence of environmental and climate change.
Sedimentary basins are also of interest due to their importance in
the exploration and recovery of natural resources, including oil
and gas, water, and industrial minerals.
The Physics of Glaciers, Fourth Edition, discusses the physical principles that underlie the behavior and characteristics of glaciers. The term glacier refers to all bodies of ice created by the accumulation of snowfall, e.g., mountain glaciers, ice caps, continental ice sheets, and ice shelves. Glaciology-the study of all forms of ice-is an interdisciplinary field encompassing physics, geology, atmospheric science, mathematics, and others. This book covers various aspects of glacier studies, including the transformation of snow to ice, grain-scale structures and ice deformation, mass exchange processes, glacial hydrology, glacier flow, and the impact of climate change. The present edition features two new chapters: "Ice Sheets and the Earth System" and "Ice, Sea Level, and Contemporary Climate Change." The chapter on ice core studies has been updated from the previous version with new material. The materials on the flow of mountain glaciers, ice sheets, ice streams, and ice shelves have been combined into a single chapter entitled "The Flow of Ice Masses."
This book is an overview of the state-of-the art developments in
sedimentology of tsunami-induced and tsunami-affected deposits,
namely tsunamiites. It also points out any problems that need
additional investigation, as well as providing insight into the
direction of future tsunamiite researches. Important
characteristics of tsunami wave and tsunami currents are explained.
There are reports on the sediments generated by recent tsunami
including the 2004 Indian Ocean tsunami presented. Tsunamiites
induced by other seismic activities, a submarine slump and a
volcanic eruption are investigated as well.
Though largely inaccessible, the geochemistry of Earth's mantle and core can be examined through a wide variety of approaches. Volume 2 focuses first on "remote" sensing using evidence from cosmochemical, seismic, petrologic and geochemical approaches. Mantle composition is then examined in detail through descriptions of mantle samples brought to Earth's surface through tectonic, volcanic, and volatile-outgassing processes. The volume concludes with examination of processes that modify the composition of the mantle and core including an early magma ocean, partial melting, element partitioning between minerals and melts, and physical mixing caused by plate subduction, mantle convection and mass exchange between mantle and core.
This book describes the structure-property-composition relationships for silicate glasses and melts of industrial and geological interest. From Antiquity to the 20th century, an introductory chapter presents this subject in a historical perspective. Basic concepts are then discussed in three chapters where attention is paid to the glass transition and its various consequences on melt and glass properties, to the structural and physical differences between amorphous and crystalline silicates, and to the mutual relationships between local order, energetics and physical properties.
Following the breakthrough in the last decade in identifying the key parameters for time and depth imaging in anisotropic media and developing practical methodologies for estimating them from seismic data, this title primarily focuses on the far reaching exploration benefits of anisotropic processing.
"Landscape Evolution in the United States "is an accessible text that balances interdisciplinary theory and application within the physical geography, geology, geomorphology, and climatology of the United States. Landscape evolution refers to the changing terrain of any given area of the Earth's crust over time. Common causes of evolution (or geomorphology-land morphing into a different size or shape over time) are glacial erosion and deposition, volcanism, earthquakes, tsunamis, tornadoes, sediment transport into rivers, landslides, climate change, and other surface processes. The book is divided into three main parts covering landscape components and how they are affected by climactic, tectonic and ocean systems; varying structural provinces including the Cascadia Volcanic Arc and California Transpressional System; and the formation and collapse of mountain systems. The vast diversity of terrain and landscapes across the United
States makes this an ideal tool for geoscientists worldwide who are
researching the country s geological evolution over the past
several billion years.
Expert petroleum geologists David Roberts and Albert Bally bring
you "Regional Geology and Tectonics: Phanerozoic Rift Systems and
Sedimentary Basins," volume two in a three-volume series covering
Phanerozoic regional geology and tectonics. Experience in analyzing
and assessing rifts-locations where the Earth s outer shell and
crust have been stretched over time by seismic activity-is critical
for you as an exploration geologist in identifying Earth s most
lucrative hydrocarbon locations in which extraction is both
efficient and safe. Vast compilations of related industry data
present regional seismic lines and cross sections, and summaries of
analogue and theoretical models are provided as an essential
backdrop to the structure and stratigraphy of various geological
settings.
This volume summarizes the results of the MARGO international working group, with the aim to develop an updated and harmonised reconstruction of sea surface temperatures and sea-ice extent of the Last Glacial Maximum oceans. The MARGO approach differs from previous efforts by developing and consistently applying measures of various aspects of reconstruction reliability, and by combining faunal and geochemical proxies.
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.
Volume 5 has several objectives. The first is to present an overview of the composition of surface and ground waters on the continents and the mechanisms that control the compositions. The second is to present summaries of the tools and methodologies used in modern studies of the geochemistry of surface and ground waters. The third is to present information on the role of weathering and soil formation in geochemical cycles: weathering affects the chemistry of the atmosphere through uptake of carbon dioxide and oxygen, and paleosols (preserved soils in the rock record) provide information on the composition of the atmosphere in the geological past.
The Neoproterozoic-Cambrian transition was a time of fundamental change in the biosphere. Between about 570 and 510 million years ago, marine organisms underwent considerable evolutionary innovation during a time of shifting ecological setting. This dramatic activity culminated in the first stratigraphic appearances of many recognizable groups of animals, an "event" often referred to as the "Cambrian explosion." In addition, there was a major change from a microbial mat-dominated sediment-water interface to a more extensively burrowed interface in shallow-marine settings. The early fossil record is a function not only of the rise or ecological diversification of marine organisms, but also the development of taphonomic and sedimentary conditions suitable for the preservation of mineralizing and nonmineralizing organisms.
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