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Anatomy of a Paleozoic Basin: The Permian Basin, USA By any standard, the Permian Basin of West Texas and New Mexico is a "super basin." With cumulative oil production of nearly 40 billion barrels (Bbbl) and annual production of nearly 2 Bbbl, it's currently one of the most important hydrocarbon-producing basins in the world. More than 29 Bbbl of this production have come from conventional (carbonate and sandstone) reservoirs, about 75 percent from carbonate reservoirs. Approximately 9-10 Bbbl of the basin's cumulative oil production have come from unconventional targets-primarily organic-matter-rich mudrocks and associated facies-during the last 10 years. The Permian Basin contains perhaps a greater volume of these mudrocks than that of any other basin, a major reason for its current global prominence among hydrocarbon-producing basins. The Permian Basin also contains one of the most extensive data sets in terms of wells drilled, cored wells, and adjacent outcrop analogs, providing a basis for studies that not only helps define the distribution of hydrocarbons but also serves as an excellent laboratory for examining basin-forming processes.This two-volume Bureau of Economic Geology Report of Investigations and AAPG Memoir contains 26 papers covering a breadth of Permian Basin topics, including 4 papers on the basin's structural geology, tectonics, and Precambrian geology; 4 papers on its paleontology and biostratigraphy; 16 on its sedimentology and stratigraphy; 1 on its reservoir systems; and 1 that provides a history and synthesis of the major depositional and deformational events that formed the basin. The goal of this set of papers is to capture, in a single publication, the wealth of information and knowledge about Permian Basin geology that has been generated over the 60 years that have passed since John Galley's early comprehensive paper on the basin in 1958.
The extinction that wiped out 95% of the living species at the end of the Paleozoic era can be explained by the fact that when it happened, all landmasses were one continent, Pangea, with an inner ocean, the Paleo-Tethys. This ocean included the richest n
In August 1990, Project 233 of the International Geological Correlation Program hosted an international conference in G6ttingen/Giessen, Germany. Discussions were focused on the Tectonothermal and Stratigraphic Evolution of the Central European Orogens. The meeting marked the first opportunity for completely open scientific exchange following the recent political reformations in central Europe. This exciting new atmosphere of international cooperation resulted in presentation of a wealth of information which was new to scientists from both sides of former political boundaries. It was apparent that a unique opportunity was available to prepare a systematic overview in a volume dealing with the geology of Central Europe. The present book represents an outgrowth of this conference, but is not merely a compilation of the papers presented in G6ttingen/Giessen. Instead, it represents a coordinated volume designed to present a balanced, comprehensive view of our present understanding of the tectonothermal and stratigraphic evolution of the Central European orogens. We gratefully acknowledge the help of the national funding agencies, who have financed much of the research work summarized in this book, and of the Interna tional Geological Correlation Programme (IGCP, project no. 233) which provided and helped to finance the organisational framework. We are indebted to Springer-Verlag for thorough copy-editing and production of this book, and we sincerely appreciate the efforts of all the reviewers whose com ments have greatly helped to improve the quality of this volume. We also thank the various contributors for their diligence and perseverance in manuscript preparation.
This is the first volume in the English language to cover the entire range of the geology of Thailand since the joint Thai-US account by Brown et al. exactly 60 years ago. Over this period there has been a phenomenal growth in interest in this core area of SE Asia. This has been led by geologists in Thailand, but with important and highly significant input from geologists based elsewhere in Asia and in Europe, Australasia and North America. Some of that research was prompted by commercial considerations, since Thailand has important energy and mineral resources, while other research has sought to understand better the stratigraphic and structural history, including the plate-tectonic story which Thailand's rocks reveal. This new volume seeks to bring together all of this knowledge into a single accessible book; it is the work of an international team drawn from Thailand, Japan, Australia, USA, Canada, Germany and the UK.
Their vastnesses concealed since an era predating the earliest mammals, two titanic chasms are uncovered beneath the canopy of modern Siberia. Lining the granite walls of the first, high above an orderly reservoir of fossilized eggs, an inscription spanning eighty-five miles describes the genome of a proto-mammalian species eradicated during the Permian Extinction. In the next, researchers discover etchings of the constellations as they would have appeared across the eons; a global timeline of ten billion years remembered and foretold by a primordial intelligence beyond our own. Armed with a genetic recipe, compelled to act by the harrowing implications of a pattern detected in the timeline, an international effort begins to return that species from extinction before mankind encounters its own. The human race has only just learned to pluck at the strings of life on Earth. Will the curtains rise on a siren's song?Where will they fall?
More than 50 years ago, the discovery of the giant Groningen Gas Field in the subsurface of the Netherlands by NAM B.V. marked a turning point in the Dutch and European energy market initiating the replacement of coal by gas. Despite the fact that the Rotliegend dryland deposits in the Southern Permian Basin are one of Europe's most important georesources, no sedimentological overview is available to date for the subsurface of the Netherlands. This SEPM Special Publication presents for the first time such a summary of the present-day knowledge, including a comprehensive core atlas from on- and offshore wells. The latter is closely linked to the series of papers in the itself, essentially providing a reference handbook for "The Permian Rotliegend of the Netherlands". Progress as a result of many scientific and consultancy studies in the Rotliegend reservoirs is summarized in this volume, with contributions covering paleogeography, depositional environment, stratigraphy, diagenesis, structural geology as well as pressure and fluid distribution in the subsurface.
This volume brings together state-of-the-art reviews of the non-biostratigraphic and biostratigraphic data that are used to define and correlate Permian time intervals. It includes analyses of Permian radio-isotopic ages, magnetostratigraphy, isotope-based stratigraphy and timescale-relevant biostratigraphy. It is the first book devoted to this subject and represents the cutting edge of Permian time-scale research.