中国显微构造地质学的回顾

我国的显微构造与组构研究始于20世纪30年代。已故何作霖教授把“岩组学”由德语文献介绍到中国，王嘉荫教授实测了国内岩石的岩组图，研究了矿物形成与变化的构造作用因素，他们把这一领域的研究与构造地质分析结合起来，结合构造地质分析引入了显微镜方法。不过在以后的30多年里，显微构造与组织分析只局限于少数学术单位和少数学者。从20世纪70年代中期开始，随着地 质工作的发展和国际交往的带动，显微构造与组构在我国得到较快速的发展。许多高校地质系开设了相关课程，在矿业开发、工程地质、环境与灾害地质等方面也得到有成效的应用。

A Review of Microstructural Geology in China

The microstructural and petrofabric analyses in China were originated in the 1930s. Prof. He introduced the petrofabric analysis from German literature to China; Prof. Wang measured and completed petrofabric diagrams of domestic rocks during the 1930s. Wang studied the tectonic interpretations of deformed rocks under the microscope in 1940. They combined the petrofabrics with tectonic dynamics, introduced application of microscopes to structural analysis for the first time in China. However, in the 30 years after that, the microstructural and petrofabric analyses were limited to a few academic institutions and a few scholars. Since the late 1970s, microstructural and petrofabric analyses have developed rapidly in China along with the development of geological work and international academic exchanges. Some related courses have been offered in many geological colleges and universities. Microstructural geology has been widely applied to mining, engineering, environmental and disaster geological work in China.