首页> 外文会议>International Symposium on Innovation amp; Sustainability of Structures in Civil Engineering(ISISS'2005); 20051120-22; Nanjing(CN) >ACHIEVEMENT, DEVELOPMENT AND CHALLENGE OF CHINESE ROCK (UNDERGROUDN) ENGINEERING 'THE RESEARCH OF ROCK MECHANICS IN 21st CENTURY IN CHINA'
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ACHIEVEMENT, DEVELOPMENT AND CHALLENGE OF CHINESE ROCK (UNDERGROUDN) ENGINEERING 'THE RESEARCH OF ROCK MECHANICS IN 21st CENTURY IN CHINA'

机译:中国岩石(地下)工程的成就,发展与挑战“ 21世纪的中国岩石力学研究”

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摘要

The research of rock mechanics and engineering must integrate with the geography and geologic environment. knowledge of Chinese rock engineering starts with chinese geography and geology environment. (1) properties of the geography the topography takes on the characteristic of echelon. And there is three echelon topography from west to east. the first echelon: The western Qinghai-Tibet plateau, its elevation is 4 000 m; the second echelon: The plateau and basin lying to the east and north of the verge of Qinghai-Tibet plateau, its elevation is 1 000-2 000 m, the third echelon; The eastern hill and plain, its elevation is less than 500 meters, the third echelon extend to the sea and forms the continental shelf near the sea. (2) the geotectonic behaviors The Earth's surface is covered by Six rigid crustal plates drifting on the asthenosphere, which moves and rotates ceaselessly. Our country lies in the Eurasian plate. Chinese mainland again can be divided into several sub-plates. (3) the distribution of the strain and stress field of the earth The deformation of the plates mainly concentrates in the verge of the plates. For our country, the deformation mainly is the verge between the Eurasia and the India plate, pacific plate. Because the plates collide mutually, crustal plates will be risen and earthquake will be caused to happen.
机译:岩石力学和工程学的研究必须与地理和地质环境相结合。中国岩石工程知识始于中国地理和地质环境。 (1)地形的性质地形具有梯队的特征。从西到东有三个梯队地形。第一梯队:青藏高原西部,海拔4 000 m。第二梯队:位于青藏高原边缘东部和北部的高原和盆地,海拔为1 000-2 000 m,为第三梯队。东部丘陵和平原,海拔不到500米,第三梯队延伸至海面,并形成靠近海面的大陆架。 (2)大地构造行为地球表面覆盖着六个在软流层上漂移的刚性地壳板,它们不断地运动和旋转。我们的国家位于欧亚板块。中国大陆又可以分为几个子板块。 (3)地球应变场和应力场的分布板块的变形主要集中在板块的边缘。对于我国而言,变形主要是欧亚大陆与印度板块,太平洋板块之间的边缘。由于板块相互碰撞,地壳板将上升并引起地震。

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