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太湖以其特殊的地貌形态、地理和行政位置,以及所起的作用,成为古往今来开发利用和科学工作者调研的重要对象。太湖成因历来众说纷纭。各派学者从地壳深源到宇宙太空、不同的侧面、立体进行解疑,从某一角度各叙其因,至今难圆其说。随着资料日益积累,工作不断深化,现代科技手段的发展,特别是现代卫照资料,结合近代考古的发现,以动态的观点来探讨太湖的成因机理,提出热力型环形构造、锥形地质体破裂,升降差异运动,造成太湖岩盆的机理模型,简称“热环锥体破裂升降”模型,来说明太湖的根本成因,及其演化运动历史过程,对解释太湖的成因,得到了进一步的启迪。一、大湖古名震泽,又名笠湖,湖泊面积2427.8平方公里,平均水深1.8米,最深2.6米,湖中大小岛屿51个,最高山峰海拔373米,高出水面370米。由于太湖作为一个环形岩块,构成岩盆的基本形态,在长
With its special topography, geographical and administrative position, and its role, Taihu Lake has become an important object of scientific research and development for all ages. Origin of the Taihu Lake has always been divided. The scholars of various schools have done so from the deep source of the crust to the space and different aspects of the universe. With the increasing accumulation of data, deepening of work, the development of modern scientific and technological means, especially the modern guarding data, combined with the discovery of modern archeology, the formation mechanism of Taihu Lake is discussed from a dynamic point of view, and the thermal ring structure, conical geological body The mechanism of Taihu rock basin, which is referred to as “hot ring cone rupture rise and fall ” model to illustrate the fundamental genesis and evolutionary history of Taihu Lake, explained the genesis of Taihu Lake and got further Inspiration. First, the ancient name of the Great Lakes Zenith, also known as Li Lake, the lake area of 2427.8 square kilometers, the average depth of 1.8 meters, the deepest 2.6 meters, 51 islands in the lake, the highest mountain 373 meters above sea level, 370 meters above the water. Since Taihu Lake as a ring rock block, constitute the basic form of rock basin in the long