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Titlebook: Arc-Continent Collision; Dennis Brown,Paul D. Ryan Book 2011 Springer-Verlag Berlin Heidelberg 2011

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樓主
發(fā)表于 2025-3-21 17:39:43 | 只看該作者 |倒序瀏覽 |閱讀模式
期刊全稱Arc-Continent Collision
影響因子2023Dennis Brown,Paul D. Ryan
視頻videohttp://file.papertrans.cn/162/161159/161159.mp4
發(fā)行地址Includes supplementary material:
學科分類Frontiers in Earth Sciences
圖書封面Titlebook: Arc-Continent Collision;  Dennis Brown,Paul D. Ryan Book 2011 Springer-Verlag Berlin Heidelberg 2011
影響因子.Arc-continent collision has been one of the important tectonic processes in the formation of mountain belts throughout geological time, and it continues to be so today along tectonically active plate boundaries such as those in the SW Pacific or the Caribbean. Arc-continent collision is thought to have been one of the most important process involved in the growth of the continental crust over geological time, and may also play an important role in its recycling back into the mantle via subduction. Understanding the geological processes that take place during arc-continent collision is therefore of importance for our understanding of how collisional orogens evolve and how the continental crust grows or is destroyed. Furthermore, zones of arc-continent collision are producers of much of the worlds primary economic wealth in the form of minerals, so understanding the processes that take place during these tectonic events is of importance in modeling how this mineral wealth is formed and preserved. This book brings together seventeen papers that are dedicated to the investigation of the tectonic processes that take place during arc-continent collision. It is divided into four sections
Pindex Book 2011
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1863-4621 ed. This book brings together seventeen papers that are dedicated to the investigation of the tectonic processes that take place during arc-continent collision. It is divided into four sections978-3-662-51876-2978-3-540-88558-0Series ISSN 1863-4621 Series E-ISSN 1863-463X
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The Subductability of Continental Lithosphere: The Before and After Story
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The Generation and Preservation of Mineral Deposits in Arc–Continent Collision Environments
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