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Titlebook: The Geology of Continental Margins; Creighton A. Burk (Chief Geologist),Charles L. Dra Book 1974 Springer-Verlag Berlin Heidelberg 1974 Ko

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書目名稱The Geology of Continental Margins
編輯Creighton A. Burk (Chief Geologist),Charles L. Dra
視頻videohttp://file.papertrans.cn/911/910495/910495.mp4
圖書封面Titlebook: The Geology of Continental Margins;  Creighton A. Burk (Chief Geologist),Charles L. Dra Book 1974 Springer-Verlag Berlin Heidelberg 1974 Ko
描述The continental margins of the world constitute the most impressive and largest physiographic feature of the earth‘s surface, and one of fundamentally great geological significance. Continental margins have been the subject of increasing attention in recent years, an interest focused by a body of new data that has provided new insights into their character. This interest was further stimulated by the realization that, in addition to the abundant living resources, continental margins contain petroleum and mineral resources that are accessible with existing technology. This realization, along with their basic geological importance, has provoked further research into the nature of continental margins throughout the world. A summary of these findings, as related to both recent and ancient continental margins, is the subject of this book. At various times in the past we had been approached individually to prepare a basic reference to continental margins; we then proposed to do such a volume jointly. However, the stimulus for the present volume eventually arose from a Penrose Conference arranged through the Geological Society of America. This conference was attended by specialists of num
出版日期Book 1974
關(guān)鍵詞Kontinentalabhang; geology; mineral; mineral resources; research
版次1
doihttps://doi.org/10.1007/978-3-662-01141-6
isbn_softcover978-3-662-01143-0
isbn_ebook978-3-662-01141-6
copyrightSpringer-Verlag Berlin Heidelberg 1974
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https://doi.org/10.1007/978-3-662-01141-6Kontinentalabhang; geology; mineral; mineral resources; research
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Creighton A. Burk (Chief Geologist),Charles L. Dra
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Book 1974dividually to prepare a basic reference to continental margins; we then proposed to do such a volume jointly. However, the stimulus for the present volume eventually arose from a Penrose Conference arranged through the Geological Society of America. This conference was attended by specialists of num
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Book 1974 great geological significance. Continental margins have been the subject of increasing attention in recent years, an interest focused by a body of new data that has provided new insights into their character. This interest was further stimulated by the realization that, in addition to the abundant
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