I. Lerche – författare
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2 produkter
2 produkter
E-bok
PDF, Engelska, 20031 543 kr
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The advent of radionuclide methods in geochronology has revolutionized our understanding of modern sedimentary processes in aquatic systems. This book examines the principles of the method and its use as a quantitative tool in marine geology, with emphasis on the Pb-210 method. The assumptions and consequences of models and their behaviour are described providing the necessary background to assess the advantages and trade-offs involved when choosing a particular model for application. One of the purposes of this volume is to disentangle the influences of complicating factors, such as sediment flux variations, post-depositional diffusion of radionuclides, and bio-irrigation of sediments, to arrive at sediment ages and to properly assess the attendant data uncertainty. Environmental impacts of chemical, nuclear, or other waste material are of concern in a variety of areas around the world today. A number of relevant examples are included, demonstrating how dating models are useful for determining sources of contaminants and interpreting their influence on the environment.The book is set at a level so that an able student or professional should have no difficulty in following the procedures and methods developed. Each chapter includes case histories showing the strengths and weaknesses of a given procedure with respect to a data example. Included with this volume is the computer source code of a new generation of modelling tools based on inverse numerical analysis techniques. This first generation of the modelling tool is included, along with detailed instructions and examples for its use, in an appendix.
E-bok
PDF, Engelska, 2017979 kr
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Dynamical Geology of Salt and Related Structures deals with many aspects of the dynamical evolution of salt bodies in sedimentary basins. This book consists of four major sections. Section A deals with salt dynamics and the motion of salt. The impact of a mobile salt mass on the structural development of the overlying formations is considered in Section B, while the development of caprock, which is commonly found overlying salt diapirs, is emphasized in Section C. The last section deliberates the interrelationships between fluid flow, salt dissolution, and heat flow in the vicinity of a salt diapir, including the connections with maturation of source rocks, migration, and trapping of hydrocarbons in salt-related structures. This publication is valuable to professional geoscientists interested in processes involved in salt dynamics.