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一 回顾显微构造研究的历史,是为了认识现在和展望未来。下面我们以偏光显微镜、费德洛夫旋转台和电子显微镜的发明及在地质上的应用,谈一下显微构造(包括构造岩石学)研究的发展过程。 第一阶段:1857年索尔贝(H.C.Sorby)将偏光镜装置于显微镜上,以研究透明矿物的光学性质。最初索尔贝在偏光镜下只研究侏罗系砂岩的薄片,后来就应用于块状结晶岩石,并且在各国迅速推广。无疑,索氏的这一重大技术改革,不仅为矿物岩石学,亦为显微构造、构造岩石学的研究,开辟了广阔的前景。1880年,克哲鲁勒夫(Kjerulf)首先依据镜下的显微
A review of the history of microstructural research is to understand the present and look forward to the future. Next, we will polarize the microscope, the invention of the Federlof rotary table and the electron microscope and its application in geology, and talk about the development of microstructure (including tectono-petrology). Stage 1: H.C.Sorby placed a polarizer on a microscope in 1857 to study the optical properties of clear minerals. Solvay first studied only the thin slices of Jurassic sandstone under the polarizer and later applied to massive crystalline rocks and rapidly promoted in various countries. Undoubtedly, this major technological reform of Soxhighes opens up a vast prospect not only for mineralogy and petrology but also for the study of microstructure and tectono-petrology. In 1880, Kjerulf first relied on microscopic microscopy