The earlier thinking for tectono-geochemistry was "the rocks enduring deformation can have chemical changes"(Sorby,1863).After a long extensive and in-depth study,some associated concepts and understandings have been proposed in tectono-geochemistry,including stress mineral,tectonic metamorphism,structural dynamic diagenetic mineralization,transformation of mineralization,tectonic facies and tectono-geochemistry.This field revealed plenty phenomena about tectonism controlling the rock formation and the deformation process,the distribution and differentiation of elements,petrogenesis,and mineralization,and at the same time promoted the development of different areas,including geotectonics,regional geology,petrology,mineral deposits,microscopic structure,geochemistry,and experimental geology.The theoretical problem is still existed in kinetic mechanism of tectono-geochemistry.Tectonic can affect the deformation of rocks,but its tectonic difference stress can not directly affect the fluid,thus can not independently constraint the process of chemical equilibrium in general.In recent years,researchers have proposed the idea of decomposing tectonic stress field,distinguishing shapes and volume and volume change of rocks,equal positive stress in different directions which caused the change of volume are called additional tectonically-induced static pressure or the additional tectonic stress.Additional tectonic stress can affect chemical reaction process,thus,it stresses more about the new field of tectono-geochemistry and promotes the theoretical development of tectono-geochemistry.Based on the progress in the tectono-geochemistry and literature analysis,the study on the tectonic combined facies and transformation with formation is the premise of the development of tectono-geochemistry,the tectonic quantification and rheology are the basis,theory and experiment are the only road of its deepening and development.Ultra-micro-nano-structure research is to construct a new level of tectonic physicochemical analysis in the developing trend of tectonic physicochemistry.