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A comprehensive single-authored book to introduce students and researchers to the marine geology of the Antarctic.
Geological information from Antarctica has so far been published in expedition reports, conference proceedings, and science journals. This information is thus not readily accessible to Earth scientists who are interested, but not directly involved, in Antarctic research. The Geology ofAntarctica bridges this gap with each chapter presenting an authoritative review of a particular aspect of Antarctic geology. The text provides descriptions of all major rock units found in Antarctica, as well as reviews of Antarctic palaeontology, geophysics, petroleum prospects, and mineral resources. Special attention is drawn to the features of Antarctica that are significant from the wider perspectives of globalgeology.
The fourth international symposium on Antarctic Earth Sciences took place in Adelaide, South Australia during the week 16-20 August 1982. This volume contains a record of the centenary activities celebrating Sir Douglas Mawson and the one hundred and seventy-four papers that were presented by delegates for discussion over the five days. Sir Douglas Mawson was part of the first team to reach the magnetic South Pole, a leading geologist and scientific figure during the heroic age of of antarctic exploration. The papers presented during the symposium were divided into fifteen categories covering east and west Antarctica, marine, land and glacial geology, plate tectonics, islands, peninsulas, climatic change and Precambrian and Cenozoic era activity. The two hundred persons from sixteen countries who attended the symposium brought together a wide range of the most current expertise and research to share, of which this volume provides a record.
The fossil history of plant life in Antarctica is central to our understanding of the evolution of vegetation through geological time and also plays a key role in reconstructing past configurations of the continents and associated climatic conditions. This book provides the only detailed overview of the development of Antarctic vegetation from the Devonian period to the present day, presenting Earth scientists with valuable insights into the break up of the ancient supercontinent of Gondwana. Details of specific floras and ecosystems are provided within the context of changing geological, geographical and environmental conditions, alongside comparisons with contemporaneous and modern ecosystems. The authors demonstrate how palaeobotany contributes to our understanding of the paleoenvironmental changes in the southern hemisphere during this period of Earth history. The book is a complete and up-to-date reference for researchers and students in Antarctic paleobotany and terrestrial paleoecology.
The present volume provides a comprehensive overview of the geology of the Antarctic continent. It is principally based on the meagre 1% of ice-free area of Antarctica and geophysical data. The only previous, fairly comprehensive treatment of Antarctic geology was published more than 25 year ago. Since then, our knowledge about the geology of the continent has increased immensely; despite the km-thick ice shield, which covers large parts of Antarcticas geology, particularly at its center. An outstanding feature of this book is that it combines the present knowledge in just one single volume. Following an introduction with a geographic outline and a general synopsis of Antarctic geology, individual chapters describe the regional geology of the seven main physiographic regions of Antarctica in detail: the Antarctic Peninsula, West Antarctica (Marie Byrd Land and Enderby Land), Transantarctic Mountains, the Shackleton Range and its surroundings (including the Bertrab, Littlewood and Moltke Nunataks), Dronning Maud Land, Lambert Glacier and the area surrounding it, East Antarctica from Kaiser-Wilhelm-II.-Land to George V Land/Terre Adélie. All seven chapters were written by acknowledged specialists in their field. Each chapter contains a topographic, historical and geological overview, a description of the respective geological units, their stratigraphy and related data and the tectonic structure of the respective region. Mostly, the findings are placed in a continent-wide/plate tectonic/geological context. The book closes with chapters on the mineral resources and the palaeontological record of the Antarctic continent. Even if the Antarctic Treaty System prohibits prospection and any exploitation of mineral resources in Antarctica at this time, occurrences of iron, other metal and coal deposits are known, and many more do probably exist. The mineral resources chapter does not just deal with known and presumed deposits, but also highlights environmental problems and relevant international treaties, economic issues and practical or general problems. The Antarctic ice is the largest fresh water resource on Earth. All nine authors are or have been active field geologists in the corresponding Antarctic regions and are affiliated with American, British, French and German research institutions. The book addresses researchers, students of geosciences, geologists and all other scientists interested in Antarctic science in general.
Antarctic Paleobiology discusses the current status of paleobiology, principally paleobotany and palynology in Antarctica, and the interrelationship of Antarctic floras to those of other Gondwana continents. It provides a broad coverage of the major groups of plants on the one hand, while on the other seeking to evaluate the vegetational history and the physical and biological parameters that influence the distribution of floras through time and space. The biologic activity is discussed within a framework of the geologic history, including the tectonic and paleogeographic history of the region. Finally, the reader will find a comprehensive bibliography of Gondwana paleobotany and palynology.