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本文拟论述的并不是“新全球构造说”或“板块构造说”这一现代的全球构造运动概念,而是概括地论述对区域的、地区的或局部的(详细的)构造进行比较的全球构造学。全球构造学是研究在1:40,000,000或更大比例尺(即最大测量范围不小于1000公里)地质图上至少可以划分出分布范围的地壳(岩石圈)构造单元。就深度来说,这些构造单元明显地属于地壳构造或深部构造的范畴,涉及到深达莫氏面的整个地壳,乃至整个岩石圈。对于地壳构造单元切忌孤立地,而应当综合地进行研究,这样才可能确切查明全球范围的规律性。
What this article intends to discuss is not a global concept of the global tectonic movement of “new global tectonics” or “tectonic tectonics,” but rather an overview of the global comparison of regional, regional or local (detailed) structures Tectonics. Global tectonics is the study of crustal (lithospheric) tectonic units that can be divided into at least one distribution on a geological map with a scale of 1: 40,000,000 or more (ie, a maximum measuring range of not less than 1,000 kilometers). In terms of depth, these tectonic units clearly belong to the category of crustal structure or deep structure, involving the entire crust, even the entire lithosphere, reaching the Mohsian plane. For the crustal structural units should not be isolated, but should conduct a comprehensive study, so as to be able to pinpoint the regularity of the global scope.