This book is intended as a comprehensive survey of the entire field of geophysical exploration. The author has endeavored to present the subject in broad perspective, emphasizing the relations, differences, common features, and, above all, the fundamentals of geophysical methods. The material is divided into two parts of six chapters each. The first part, written in elementary language, addresses those desiring an insight into the working principles and geological applications of geophysical methods. It is intended for individuals in executive and geologic advisory capacity and for persons not directly concerned with field or laboratory operations.

Unprecedented advances in geophysics during the 1970s and 1980s have revolutionized our concepts about the Earth. This scientific revolution is largely a consequence of the discovery of seafloor spreading and the subsequent formulation of the theory of plate tectonics. In addition, however, the exploration of the Moon and planets has had a profound impact upon geophysics, as has the development of innovative space technologies, where orbiting satellites have yielded a wealth of new and truly global geophysical data. A vital catalyst for these great advancements in knowledge has been the astonishing growth of computer technology, with the attendant development of powerful new digital techniques for collecting, processing, and analyzing massive quantities of digital data. The overall effect has been to alter foreover not only our understanding of the Earth but also the fundamental way in which we do geophysical research.

Geophysics, as its name indicates, has to do with the physics of the earth and its surrounding atmosphere. Gilbert’s discovery that the earth behaves as a great and rather irregular magnet and Newton’s theory of gravitation may be said to constitute the beginning of geophysics. Mining and the search for metals date from the earliest times, but the scientific record began with the publication in 1556 of the famous treatise De re metallica by Georgius Agricola, which for many years was the authoritative work on mining.

This book is intended as a comprehensive survey of the entire field of geophysical exploration. The author has endeavored to present the subject in broad perspective, emphasizing the relations, differences, common features, and, above all, the fundamentals of geophysical methods. The material is divided into two parts of six chapters each. The first part, written in elementary language, addresses those desiring an insight into the working principles and geological applications of geophysical methods. It is intended for individuals in executive and geologic advisory capacity and for persons not directly concerned with field or laboratory operations. 

It is now 10 years since the Encyclopedic Dictionary of Exploration Geophysics was published. In this edition new terms have been added and definitions revised in order to keep up with the technological advances of this decade. 
The first edition appeared when exploration geophysicists were starting to cope with data processing and help was needed with the processing vocabulary.

All information about the Earth’s interior comes from field observations and measurements made within the top few kilometers of the surface, from laboratory experiments and from the powers of human deduction, relying on complex numerical modeling. Solid Earth Geophysics encompasses all these endeavors and aspires to define and quantify the internal structure and processes of the Earth in terms of the principles of physics, corresponding mathematical formulations and computational procedures.

Submarine Landslide Deposits in Orogenic Belts
Submarine Landslide Deposits in Orogenic Belts: Olistostromes and Sedimentary Melanges
Kei Ogata, Andrea Festa, Gian Andrea Pini, and Juan Luis Alonso    
Mass-Transport Deposits in the Foredeep Basin of the Miocene Cervarola Sandstones Formation (Northern Apennines, Italy)
Alberto Piazza and Roberto Tinterri    
Late Miocene Olistostrome in the Makran Accretionary Wedge (Baluchistan, SE Iran):
A Short Review
Jean-Pierre Burg    
Spatial Distribution of Mass-Transport Deposits Deduced From High-Resolution Stratigraphy:
The Pleistocene Forearc Basin (Boso Peninsula, Central Japan)

The deposit is situated in southeastern New South Wales at Lat.35°04*S, Long.1A9°34*E. (Fig.l) The first phase of testing proved up a body of poljmietallic massive sulphides and an adjacent zone of dominantly copper ore. The massive sulphides body consisted of about 6.3 million tonnes of copper, lead and zinc ore (1.7% Cu: 5.5% Pb; 14.4% Zn) and was the main target for geophysical investigation. The copper ore zone contains about 3.7 million tonnes averaging about 1.9% Cu, 0.1%Pb, 0.5% Zn in a number of ore shoots both along strike from and below the massive sulphides. Subsequent drilling indicated several concealed bodies of massive sulphides, separate from the first discovered body but these are at depths of more than 200m and hence too deep to have influenced the geophysical investigations.  <...>

Often times a student is introduced to geophysics as a rather specialized branch of geology, employed only for prospecting or in graduate research. Geophysics courses are usually taken later in a college schedule after adequate preparation in physics and mathematics. Because it is a broad, interdisciplinary area of physical science, one can obtain a background in geophysics by taking selected studies in several different but related fields.