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一、前言欧洲地壳构造演化的发展,大致呈从北到南演变更替发展的趋势。因此,其大地构造单元划分从北到南大致是:前寒武纪区(如芬兰、丹麦、挪威),加里东运动区(如英国、德国等),海西运动区(如法国、西班牙等),阿尔卑斯运动区(如瑞士、意大利、奥地利、南斯拉夫等)。经广泛而强烈的海西褶皱造山运动,从晚石炭世到早二叠世,除南部边缘仍为海域(古地中海)外,几乎整个欧洲隆起成陆,结束了广泛海槽发育的历史。特别是在西欧,这一构造运动表现尤为突出。该造山运动的影响表现
I. Preface The development of the crustal tectonic evolution in Europe shows a general trend of evolution from north to south. Therefore, its tectonic unit division from north to south roughly is: Precambrian (such as Finland, Denmark, Norway), Caledonian sports areas (such as the United Kingdom, Germany, etc.), Hercynian sports areas (such as France, Spain, etc. ), The Alps sports area (eg Switzerland, Italy, Austria, Yugoslavia, etc.). Extensive and intense Hercynian fold orogeny, from the Late Carboniferous to the Early Permian, covered almost all of Europe with the exception of the southern margin of the sea (paleo Mediterranean), ending the history of widespread trough development. This tectonic movement is particularly prominent in Western Europe, in particular. The performance of the orogeny