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Books > Earth & environment > Earth sciences > Structure & properties of the Earth
An Introduction to Mining Seismology describes comprehensively the
modern methods and techniques used to monitor and study seismicity
and rockbursts in mines. Key case histories from various worldwide
mining districts clearly illustrate and skillfully emphasize the
practical aspects of mining seismology. This text is intended as a
handbook for geophysicists and mining and rock mechanics engineers
working at mines. It will also serve as an essential reference tool
for seismologists working at research institutions on local
seismicity not necessarily induced by mining.
Piton de la Fournaise and Karthala are both shield volcanoes in the southwest Indian Ocean. This publication summarizes the work done on these very active basaltic volcanoes. Piton de la Fournaise has a long history of scientific research and monitoring, with many data collected during recent eruptions. It is certainly one of the most studied volcanoes in the world. The work presented in this monograph includes geological, geophysical, geochemical and petrological aspects, but also studies on physical geography, natural hazards and the sociological and behavioural approaches.' The Karthala volcano may be less well known, but it serves as an interesting comparison to Piton de la Fournaise. Although situated close to the volcanoes of Hawaii, it differs from them by its more alkaline magmas and less frequent activity. It was also monitored for more than 25 years, producing extraordinary eruptions in recent years.
Tsunamis in the European-Mediterranean Region: From Historical Record to Risk Mitigation provides readers with a much needed, reliable, and up-to-date history of the region, including descriptions and parameters of the main events from pre-history to the present that are supported by parametric catalogues, pictorial material, and examples of instrumental records, such as tide-gauge records. The book presents a broader perspective of needed action for local and national governments, and international organizations, and is written by an internationally recognized expert in this field, providing an authoritative account of historical tsunamis in the eastern Mediterranean. It addresses key points of tsunami mitigation, including the systems currently available for tsunami recording, monitoring, and early warning, along with a presentation of the preventative measures that can be applied in all tsunami-vulnerable regions.
This volume presents different studies carried out on induced seismicity, both from experimental and theoretical viewpoints. Several examples of seismic activity induced by underground nuclear explosions, impoundment of artificial reservoirs, and mining activities are given and discussed. Another important subject which is covered is earthquakes induced by other large earthquakes. Further, tectonic stress release in the immediate vicinity of an underground nuclear explosion is treated. The release produces aftershocks of small magnitude, usually for several weeks, occurring a few kilometers within the shot point. This phenomenon is of importance in the context of monitoring a Comprehensive Test Ban Treaty.
"Earthquake Hazard, Risk and Disasters" presents the latest
scientific developments and reviews of research addressing seismic
hazard and seismic risk, including causality rates, impacts on
society, preparedness, insurance and mitigation. The current
controversies in seismic hazard assessment and earthquake
prediction are addressed from different points of view. Basic tools
for understanding the seismic risk and to reduce it, like
paleoseismology, remote sensing, and engineering are
discussed.
This book provides a comprehensive description of the volcanological, petrological and geochemical features of the Poas Volcano (Costa Rica), one of the most active volcanic systems in Central America and part of the Central America Volcanic Arc (CAVA). Poas Volcano hosts a unique sulfur lake, which actually is one of the world's most acidic lakes, and has experienced molten sulfur eruptions. Past investigations, current monitoring activities and planned programs of investigation into lessening of the volcanic hazard are reported here. Specific sections of the monograph will be devoted to the impact of this volcano on the social, agricultural and industrial activities in the area. Legends and popular traditions related to this volcano will be described in the last chapter to round up a complete scientific review on this unique volcanic system.
"Earthquakes and Coseismic Surface Faulting on the Iranian Plateau" is a comprehensive and well-illustrated multi-disciplinary research work that analyzes the human and physical aspects of the active faults and large-magnitude earthquakes since ancient times on the Iranian Plateau. The long-term historical, archaeological, and sociological record of earthquakes discussed here gives insight into earthquake magnitudes, recurrences, fault segmentation, clustering, and patterns of coseismic ruptures from prehistoric times to the present. The first part of the book examines oral traditions and literature of the region concerned with earthquakes, particularly in folklore, epic literature, and theology. The second part assesses dynamic phenomena associated with earthquakes, including active tectonics, archaeoseismicity, and coseismic surface faulting throughout the twentieth century. This work is a valuable technical survey and an essential
reference for understanding seismic hazard analysis and earthquake
risk minimization in earthquake-prone developing and developed
countries throughout the world.
Presenting current approaches in observational and computational seismology, this book introduces advanced methods and techniques by means of case studies in earthquake research. Among others these include solving inverse seismologic problems, tomography for structure imaging, characterizing fault damage and healing, seismicity analysis for determining pre-shock moment release, and coupled solid-fluid models.
Authored by a geophysicist with more than 50 years of experience
in research and instruction, "Reflection Seismology: Theory, Data
Processing and Interpretation" provides a single source of
foundational knowledge in reflection seismology principles and
theory. Reflection seismology has a broad range of applications and
is used primarily by the oil and gas industry to provide
high-resolution maps and build a coherent geological story from
maps of processed seismic reflections. Combined with seismic
attribute analysis and other exploration geophysics tools, it aids
geologists and geo-engineers in creating geological models of areas
of exploration and extraction interest. Yet as important as
reflection seismology is to the hydrocarbon industry, it s
difficult to find a single source that synthesizes the topic
without having to wade through numerous journal articles from a
range of different publishers. This book is a one-stop source of
reflection seismology theory, helping scientists navigates through
the wealth of new data processing techniques that have emerged in
recent years.
Teide Volcano has many different meanings: For the Guanche aborigines, who endured several of its eruptions, it was Echeide (Hell). Early navigators had in Teide, a lifesaving widely visible landmark that was towering over the clouds. For the first explorers, Teide was a challenging and dangerous climb, since it was thought that Teide's peak was so high that from its summit the sun was too close and far too hot to survive. Teide was considered the highest mountain in the world at that time and measuring its height precisely was a great undertaking and at the time of global scientific significance. For von Buch, von Humboldt, Lyell and other great 18th and19th century naturalists, Teide helped to shape a new and now increasingly 'volcanic' picture, where the origin of volcanic rocks (from solidified magma) slowly casted aside Neptunism and removed some of the last barriers for the development of modern Geology and Volcanology as the sciences we know today. For the present day population of Tenerife, living on top of the world's third tallest volcanic structure on the planet, Teide has actually become "Padre Teide", a fatherly protector and an emblematic icon of Tenerife, not to say of the Canaries as a whole. The UNESCO acknowledged this iconic and complex volcano, as "of global importance in providing evidence of the geological processes that underpin the evolution of oceanic islands". Today, 'Teide National Park' boasts 4 Million annual visitors including many 'volcano spotters' and is a spectacular natural environment which most keep as an impression to treasure and to never forget. For us, the editors of this book, Teide is all of the above; a 'hell of a job', a navigation point on cloudy days, a challenge beyond imagination, a breakthrough in our understanding of oceanic volcanism that has shaped our way of thinking about volcanoes, and lastly, Teide provides us with a reference point from where to start exploring other oceanic volcanoes in the Canaries and beyond. Here we have compiled the different aspects and the current understanding of this natural wonder.
The first work of its kind, "Volcanic Reservoirs in Petroleum Exploration" summarizes the current research and exploration techniques of volcanic reservoirs as a source of oil and gas. With a specific focus on the geological features and development characteristics of volcanic reservoirs in China, it presents a series of practical exploration and evaluation techniques based on this research. Authored by an award-winning petroleum geologist, it introduces exploration and outcome prediction techniques that can be used by scientists in any volcanic region worldwide. Volcanic reservoirs as new sources of petroleum resources are a
hot topic in petroleum exploration. Although volcanic rock cannot
generate hydrocarbons, it can serve as a reservoir for hydrocarbons
when conditions permit. This book explains the differences between
volcanic reservoirs and other major reservoir types, and describes
effective methods for examining volcanic distribution and
predicting volcanic reservoirs, providing a framework for
systematic studies throughout the world.
This edited volume is an up-to-date guide for students, policy makers and engineers on earthquake engineering, including methods and technologies for seismic hazard detection and mitigation. The book was written in honour of the late Professor Jai Krishna, who was a pioneer in teaching and research in the field of earthquake engineering in India during his decades-long work at the University of Roorkee (now the Indian Institute of Technology Roorkee). The book comprehensively covers the historical development of earthquake engineering in India, and uses this background knowledge to address the need for current advances in earthquake engineering, especially in developing countries. After discussing the history and growth of earthquake engineering in India from the past 50 years, the book addresses the present status of earthquake engineering in regards to the seismic resistant designs of bridges, buildings, railways, and other infrastructures. Specific topics include response spectrum superposition methods, design philosophy, system identification approaches, retaining walls, and shallow foundations. Readers will learn about developments in earthquake engineering over the past 50 years, and how new methods and technologies can be applied towards seismic risk and hazard identification and mitigation.
This book presents an analysis of our current knowledge on the origin of the Earth's continental crust. There are two aspects to consider: tectonic and igneous processes. Tectonic aspects include sedimentary accretion, terrane accretion, and continental collision at continental margins, in association with plate subduction. These processes result in the formation of large mountain belts, the building up of which literally grows the continents. However, these tectonic aspects are concerned with material recycling within the crust, and hence do not contribute to volumetric growth of continental crust. Igneous processes concern separation of continental crust from the mantle and result in the volumetric growth of continental crust. Therefore, the main focus of this book is to systematically examine why and how the Earth's continental crust forms, by evaluating magmatic processes at island arcs where new continental crust forms.
The book covers multi-disciplinary topics in observational, computational and applied geophysics in aspects of solid earth system. The authors provide an up-to-date overview for methods and techniques in seismology, with a focus on fault structure, strong ground motion and earthquake forecast based on full-3D earth structure models. Abundant of case studies make it a practical reference for researchers in seismology and applied geophysics.
This analysis of the aftermath of earthquakes in Japan, Turkey and India reveals important insights into how the outcome of each was affected by the different styles of state-society relationships. Using a comparative approach the book also seeks to draw out patterns and lessons that can be applied more generally to societies in the aftermath of such events. The result is a groundbreaking work that will be of major importance to all those whose work involves them in dealing with the aftermath of disasters and major conflict
The critically acclaimed serialized review journal for over 50 years, "Advances in Geophysics" is a highly respected publication in the field of geophysics. Since 1952, each volume has been eagerly awaited, frequently consulted, and praised by researchers and reviewers alike. Now in its 52nd volume, it contains much material still relevant today--truly an essential publication for researchers in all fields of geophysics.
The dynamics of the earthquake rupture process are closely related
to fault zone properties which the authors have intensively
investigated by various observations in the field as well as by
laboratory experiments. These include geological investigation of
the active and fossil faults, physical and chemical features
obtained by the laboratory experiments, as well as the
seismological estimation from seismic waveforms. Earthquake dynamic
rupture can now be modeled using numerical simulations on the basis
of field and laboratory observations, which should be very useful
for understanding earthquake rupture dynamics. |
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