The study of paleo-rheological properties of rocks is one of important aspects of continental dynamical research. One way of quantitative research on paleo-rheology of rocks is to estimate rock rheological parameters in the just physical-chemical environment in which rocks deformed, through measurement of geometric parameters of natural structural deformation of rocks in the quantitative connection, which is established by scale-model, of rock rheological parameters and geometric parameters of natural structural deformation. This paper introduces the advances of study on quantitative research on natural deformed rocks in methods of structural measurement.