The Sedimentary Basins of the United States and Canada


Book Description

In recent years there have been rapid strides in our understanding of plate-tectonic processes, many developments in methods of basin analysis, and the accumulation of much new surface and subsurface geological and geophysical data. Projects such as COCORP (in the United States) and Lithoprobe (in Canada) have provided essential insights into the deep crustal structure of the continent. Synthesis of all the available information about North America's geological regions has not been attempted systematically since the "Decade of North American Geology project undertaken by the Geological Society of America and the Geological Survey of Canada nearly twenty years ago. The book commences with a summary of the Phanerozoic geological history of the United States and Canada, illustrated with a suite of new paleogeographic maps, and tying in each of the subsequent regional chapters by the inclusion of numerous cross-references. This followed by a set of fifteen regional syntheses of the principal tectonic regions of the United States and Canada, focusing on the stratigraphic and tectonic history of the major sedimentary basins. Most of these chapters have been contributed by specialists, drawing on their own research, and providing interpretive summaries of a type not previously attempted. - Up-to-date synthesis of the sedimentary/tectonic history of the major areas of the United States and Canada - Up-to-date references - Many new color maps







Biology Pamphlets


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Melanges


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Geologic History of the Feather River Country, California


Book Description

How did the Sierra Nevada and adjacent lands come to be the size and shape they are today? This book covers 400 million years of physical evolution in a language understandable to nonscientists, tracing the volcanic activity, the folding and building of mountains, the breaking of blocks along fault lines, and the work of erosion and glaciers that have created today's dramatic landscape. Cordell Durrell spent a lifetime reading this complex story of movement and change in the rocks of the Feather River country. He shares with readers the excitement of discovering by remote but careful inference what must have happened millions upon millions of years ago. The basic methods of geologic analysis that Durrell describes can be applied anywhere on the earth's surface, lending new fascination to our travels throughout the frozen arctic, dry deserts, tropical rainforests, low swamps, and high mountains like California's magnificent Sierra.




Petroleum Accumulation Zones on Continental Margins


Book Description

Much of the world’s petroleum is located on continental margins, and any further development of these offshore deposits would be impossible without new technologies and new methods contained in this volume. Written by some of the world’s foremost authorities on oil and gas, this volume explains for the practicing engineer and the engineering student some of the most important and cutting-edge techniques for developing offshore fields on continental margins.




The Explorer’s Guide to Death Valley National Park, Second Edition


Book Description

Originally published in 1995, soon after Death Valley National Park became the fifty-third park in the U.S. park system, The Explorer's Guide to Death Valley National Park was the first complete guidebook available for this spectacular area. Now in its second edition, this is still the only book that includes all aspects of the park. Much more than just a guidebook, it covers the park's cultural history, botany and zoology, hiking and biking opportunities, and more.







Late Jurassic Margin of Laurasia—A Record of Faulting


Book Description

"The objective of this volume is to characterize geologic relationships and settings at the margin of the Laurasia plate from Middle Jurassic to the Early Cretaceous, overlapping the time of the opening of the central Atlantic basin, with the intent of assessing the compatibility of the features with contemporaneous, sinistral fault movement"--Introduction, page v.