New Perspectives on the Caledonides of Scandinavia and Related Areas
New Perspectives on the Caledonides of Scandinavia and Related Areas
复制标题
斯堪的纳维亚喀里多尼德及相关地区的新视角
作者：
F. Corfu;D. Gasser;D. Chew
加里东山脉是一个主要的造山带，从北极延伸，通过斯堪的纳维亚半岛，东格陵兰岛，英国和爱尔兰进入北美的大西洋海岸。随着Rodinia的分裂，加里东大陆在古生代由各大陆漂移形成，并最终在志留纪和泥盆纪聚集。造山带随后在大西洋打开期间分裂。本卷汇集了25篇论文，介绍了现代研究的结果，这些研究调查了造山过程和该带特定组成部分的起源。这些贡献反映了不同的研究方向，将传统的实地研究与现代分析技术联系起来。此外，三个概述文件总结了在斯堪的纳维亚半岛，斯瓦尔巴特群岛，东格陵兰岛，英国和爱尔兰带的主要特征，突出了自30年前的斯堪的纳维亚加里东的最后一次重大合成所取得的进展，并讨论了重要的开放性问题。
The Caledonides are a major orogenic belt that stretches from the Arctic, through Scandinavia, East Greenland, Britain and Ireland into the Atlantic coast of North America. Following the break-up of Rodinia, the Caledonides formed in the Palaeozoic by the drifting of various continents and their eventual aggregation in the Silurian and Devonian. The orogen subsequently fragmented during the opening of the Atlantic Ocean. This volume brings together 25 papers presenting the results of modern research that investigates the orogenic processes and the provenance of specific components of the belt. The contributions reflect different lines of research, linking traditional field studies with modern analytical techniques. In addition three overview papers summarize the main features of the belts in Scandinavia, Svalbard, East Greenland, Britain and Ireland, highlighting the advances made since the last major synthesis of the Scandinavian Caledonides 30 years ago, and discussing important open questions.