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Progress in the study of tectophysicochemistry

Progress in the study of tectophysicochemistry
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摘要 Tectophysicochemistry is a research area that deals with the interrelations between physical and chemical changes of crustal materials caused by tectonism. A given tectonic force may be resolved into two parts: homogeneous stress and differential stress. Homogeneous stress refers to isotopic pressure, which is superimposed on the original pressure and affects the equilibrium of various chemical reactions. It is also a factor that influences petrogenesis, metallogenesis and metamorphism. Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features. Tectophysicochemistry pays special attention to pressure, temperature and other physicochemical conditions produced or induced by tectonism and studies the influences of additional tectonic parameters on various chemical equilibria, so it gradually develops into an independent area of science. Tectophysicochemistry is a research area that deals with the interrelations between physical and chemical changes of crustal materials caused by tectonism. A given tectonic force may be resolved into two parts: homogeneous stress and differential stress. Homogeneous stress refers to isotopic pressure, which is superimposed on the original pressure and affects the equilibrium of various chemical reactions. It is also a factor that influences petrogenesis, metallogenesis and metamorphism. Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features. Tectophysicochemistry pays special attention to pressure, temperature and other physicochemical conditions produced or induced by tectonism and studies the influences of additional tectonic parameters on various chemical equilibria, so it gradually develops into an independent area of science.
作者 Lü Guxian
出处 《Chinese Science Bulletin》 SCIE EI CAS 2003年第11期1069-1079,共11页
基金 This work was supported by the Project 2002201 of the Ministry of Land and Resources Scientific and Technological Development Plan,the Scientific and Technological Mineral Prospecting Project of the State Development Planning Commission(Grant No,JG9471 l0) the Fundamental Research Special Support Project of the Ministry of Science and Technology of China(Grant No.GJ94-83) Geological Survey Project(Grant No,20023046) the State Climbing Projects(Grant Nos.G1999043214 and 95-39Yu-6-3).
关键词 地壳运动 地壳物质 物理变化 化学变化 构造物理化学 岩石形成 构造运动 tectophysicochemistry, additional tectonic stress-induced hydrostatic pressure, calculation of corrected depth, additional tectonic parameter, tectochemistry, mineralizational geological event.
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