Bøger i Cambridge Earth Science Series serien

This 1980 book shows the positions of the major continental areas during the past 560 million years as four series of computer-drawn maps, which provide a framework on which a wide variety of data may be plotted. Cylindrical equidistant and Lambert equal-area polar projections are used, with a thirty-degree latitude-longitude grid.

This 1983 volume is concerned with the features of and the laws governing the occurrence of water in the interior of the Earth. Special attention is paid to the origin of the water in the interior of the Earth, its movements and its changes of state.

Mr Hughes argues that approaches (previous to 1976) to the evolutionary origin and early history of or flowering plants have been inadequate and misleading. He suggests that the date is in the Cretaceous period and there is a good chance of ancestors being found if other fossil plants of that period are studied.

This book was originally published in 1970. Writing from the viewpoint of a geologist rather than a chemist, the author outlines the geologically important organic compounds and their reactions, as well as the fundamental analytical methods used in organic chemistry. This book will be useful to anyone with an interest in non-marine organic geochemistry.

This textbook describes the physics of the plastic deformation of solids at high temperatures. It is directed at geologists or geophysicists interested in the high-temperature behaviour of crystals who wish to become acquainted with the methods of materials science in so far as they are useful to earth scientists.

One of four volumes which provides a good understanding of the mode of occurrence, geological setting and phosphogenesis of the world's phosphate resources.

This 1985 book examines the origin of the present diversity of marine invertebrate animals. A review of the early stages in the history of life discussing the time-scale of the relevant geological periods alongside corresponding events in the evolutionary sequence is followed by an overview of the early diversification of marine life.

This 1977 book shows the positions of the major continental areas during the past 220 million years as four series of computer-drawn maps. All the maps are based on quantitative geophysical or topographic information: paleomagnetic pole positions, ocean floor magnetic anomalies, and best fits of the continental margins.

In this 1981 substantial work, M. J. Hambrey and W. B. Harland have assembled essays by leaders in the field of pre-Pleistocene glacial research. The work's various chapters review in depth the glacial records of Africa, Antarctica, Asia, Australasia, Europe, and North and South America.

This 1973 comprehensive catalogue examines the many presences and absences found within the characteristics of different types of quartz grain sand. The focal point of this work is the numerous micrographs, selected specifically for their ability to demonstrate the many variations in the surface textures of quartz grain sand.

The main goal of this book is to review in detail the advances, which existed at the time, in the interpretation of Jurassic facies in the classical European and American deposits and to then apply this knowledge to illuminate more general topics such as the fluctuation in land/sea distribution and the nature of the Jurassic climate and biogeography.

This book examines the environmental setting and resulting phosphorites which formed during the Miocene period.

This comprehensive synthesis of our knowledge of the biostratigraphy of marine plankton is the work of an international team of eighteen authors. It covers all the major fossil groups that can be used to date sediments and rocks in the time interval Late Mesozoic to Holocene.

This comprehensive synthesis of our knowledge of the biostratigraphy of marine plankton is the work of an international team of eighteen authors. It covers all the major fossil groups that can be used to date sediments and rocks in the time interval Late Mesozoic to Holocene.

This study of the historical seismicity of Iran over the last thirteen centuries shows that patterns of seismic activity change over time, and also reveals a long-term tectonic pattern which is different from that deduced from short-term observations. The historical data provides the basis for the development of earthquake prediction models and for long-term earthquake hazard assessment.

This unique survey describes the world's ancient phosphorite deposits on a scale never previously attempted. The International Geological Correlation Programme started Project 156, on world phosphate resources, in 1977. It is expected that the final results of the project will be published as four reference volumes, of which this is the first.