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本文从沉积建造、构造类型、结合岩相厚度的分析以及与鄰区地槽在地质构造上的形成和发展,讨论了浙西地区大地构造性质,並把它归属於华南加里东地槽褶皱区的浙西、皖南加里东地槽系的内部继承地槽拗陷,在这个地槽内又划分出四个构造——建造带。同时本文也论述了本区褶皱构造的成因,地壳构造形成和发展的两种形式——继承与上迭构造等问题。此外,也涉及到与上述问题有关的地槽褶皱作用的问题,在空间上地槽褶皱作用具有从两侧向中间迁移的发展历史,在时间上地槽褶皱作用远远落后於地槽沉积建造的结束,以及在同一地槽内地槽“封闭”具有不同形式的问题。
Based on the analysis of sedimentary structures, types of structures, thickness of lithofacies combined with the formation and development of geological structures in the adjacent troughs, this paper discusses the tectonic features of the western Zhejiang Province and places it in the crust zone of the Galliferong in South China Of the western Zhejiang, southern Anhui Caledonian trough system inherits the trough depression, in this trench and divided into four structures - construction zone. At the same time, this paper also discusses the causes of fold structure in this area, the formation and development of crustal structure of two forms - inheritance and the Diego Diego structure and other issues. In addition, it also involves the problem of the geosynclinal fold related to the above-mentioned problems. The tectonic evolution of the geosynclinal fold from the two sides to the middle of the geosynclinal fold has spatially lagged behind the geosynclinal sedimentation , And the problem of different forms of “closure” of the trough in the same trough.