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亚洲地壳根据地层沉积类型和生物区系可分六大区:三个稳定区是北亚大陆区、中轴大陆区和南亚大陆区,基底固结都在距今1,800百万年前,三个活动区是北亚陆间区、南亚陆间区和环太平洋陆缘区,都由不同时代的褶皱区和前古生代中间地块组成,地壳构造发展根据运动强化期分为5个阶段:前阜平阶段(陆核形成)、阜平吕梁阶段(原地台形成)、吕梁晋宁阶段(地台形成)、晋宁印支阶段(大陆主体形成)和后印支阶段(现大陆轮廓形成),文中并简单讨论了地下不同深度的滑移运动与地表不同类型构造之间的可能关系。
The Asian crust can be divided into six regions according to the sedimentary types and biota of the strata: the three stable regions are the North Asia continent, the central axis continent and the South Asia continent. The consolidation of the basement occurred 1,800 million years ago and three The active area is composed of the North Asia land area, the South Asia land area and the Pacific Rim land area, which are composed of the fold areas in different epochs and the pre-Paleozoic middle blocks. The development of the crustal structure is divided into five stages according to the period of exercise enhancement: (The formation of the original platform), the Jinning stage of Lüliang (platform formation), the Indosinian phase of Jinning (the formation of the main body of the mainland) and the post-Indosinian phase (the continent contours are now formed) In this paper, we briefly discuss the possible relationship between slip movement at different depths and different types of structures on the ground surface.