OV brief biography
Back a brief biography of Korzhinsky was born D. Korzhinsky see a large Soviet encyclopedia, who died next year after the birth of his second son. Children received education at the level of high school from their mother. A year before the exterior in the eighth grade of the real school, Mitya was preparing with coming teachers. The end of the school was the first year of the Civil War in Mitya worked as a foreman in the survey party in the low -land tundra of the Kola Peninsula, which ended up in the occupation of English interventionists.
Party staff were mobilized into the counter-revolutionary army, in which Dmitry Sergeyevich served as an ordinary telephonist. In February, in it, D. after passing exams for the 1st year of the Leningrad Mining Institute D., as a 2nd year student, was released from military service. At the institute, D. Bilibin studied the greatest influence on D., with which he retained the friendship to the death of the latter.
According to D., in any political parties and organizations, D. departed from religious beliefs after he was robbed during an excursion to the Orthodox places of the Solovetsky monastery by the son of a major religious figure of the Urals, who, the complaint of D. In the real school of D. at the same time, from G. to the GG. In e gg.
Korzhinsky, with the active participation of his student and future academician of the Russian Academy of Sciences V., was replaced by V. in Siberia D. But the scientific results turned out to be more valuable. Such components are called “completely mobile components” in the thermodynamic sense Korzhinsky, the intensive factors of the systems of their chemical potentials, activity or concentrations are associated with quite mobile components, and therefore these components do not determine the number of phases of the system of the system, therefore, in partly open systems, which include all metasomatic and magmatic formations, the maximum number, maximum number Minerals cannot exceed the number of thermodynamically inert components.
This form of phases rule is called “the mineralogical rule of the Korzhinsky phases. From this point of view, mainly the two- and three-mineral composition of metasomatic breeds is very easily explained. During these years, D. Korzhinsky was the first to develop the criteria of the deepness of metamorphic facies by analyzing the stability of sa-containing aluminosilicates, dependent on the MG and FE distribution temperature between silicates.
According to Dmitry Sergeyevich, the period of studying the phlogopite deposits was the happiest in his scientific life, when ideas were born one after another. The main achievements of this period, together with the theoretical justification of the differential mobility of the components, are outlined in its well -known monograph “Theoretical Fundamentals of the analysis of mineral paragenesis” but later D.
Korzhinsky put forward a significant amount of brilliant hypotheses, which formed the basis for the development of the theory of metasomatism, magmatism and ore formation. The first time was the discovery of the principle of completely mobile behavior in the magician alkalis with the development of alkaline criteria Magm Korzhinsky, which was supplemented by a hypothesis of transmagmatic fluid streams in Magmas Korzhinsky, at the exit from magma into the internships, these fluids give rise to metasomatosis of the magmatic stage with a magmatic substitution, for example, by the gradualization of the border, for example, by the gradualization of The rear area of the metasomatic column.
Later, D. in the field of metasomatism D. The basis for this was the constant presence of maximum acidity metasomatitis, for example, quartz veins of a granite formation, regarding which all metasomatitis can be divided into metasomatitis of the early-base and late-base stages. Such the evolution of metasomatic processes is associated with the acid-base interaction of the components in solutions depending on the temperature of Korzhinsky, and other work.
This concept has discovered the possibilities for creating a genetic classification of Korzhinsky metasomatitis, based on the concept of metamagmatic interaction of magma with transmagmatical fluids, see that this relationship is due to the redistribution of ore components between magma and transmagmatical fluids in metamagmatic interaction in parallel with the possibility of a certain components of some components fluid streams.
Outstanding scientific achievements brought Korzhinsky recognition both in their own country and abroad. Korzhinsky successfully defended his doctoral dissertation. Korzhinsky was also the vice president of the International Mineralogical Association to the city of Korzhinsky was elected an honorary member of many foreign scientific academies and societies. Korzhinsky was awarded the Golden Star and the title of Hero of Socialist Labor G.