Kuznetsov, Anatoly Alexandrovich

He graduated from the Department of Petrography (1962) and correspondence postgraduate study (1967) at the Geological Faculty of St. Petersburg State University (former Leningrad State University). Candidate of Geological and Mineralogical Sciences (1968). As a student, he began his research and production activities at VNIIOkeangeologiya (formerly NIIGA), participating (1960-1965) in state geological surveying on a scale of 1: 200000 of the Tunguska trap province of the Siberian platform and analyzing the features of mafic magmatism of the Northern Verkhoyaniye (1965-1966). ) Then, while working at VSEGEI (1967–1999), he conducted case studies on the geology, petrology, geochemistry, and ore content of magmatic and protocrystal (“regional metamorphic”) formations using the example of the orogenic zones of Central Asia (Pamir, Tien Shan), an autonomously activated region in the south of the Far East (Amur, or Khingano-Bureinskaya) and ancient shields (Anabar, Aldan). He is a co-author (N.G. Vlasov and A.A. Kuznetsov) of the first "Pamir Structural-Formative Map" of 1: 500000 scale (1969, VSEGEI funds), one of the co-authors of "Forecast-metallogenic maps for uranium in a number of regions of the south of the Far East "Scales of 1: 1,000,000 and 1: 200,000 (1975, 1978, ibid.), Author of the" Structural-facies map of the crystalline basement of the Aldan-Stanovoi geostructure "of scale 1: 1500000 (1988, 1993, ibid.) And the first" Structural-facies-formation map of the Anabar shield ”scale 1: 500000 (1993, ibid.) From the perspective of the protocrystal primary nature of the Early Precambrian bark oh. Main research interests: petrogenesis of lithospheric global crystalline subshells and regional crystalline layers (geolins) - parageneses of protocrystal and erupted geoformations of the main tectonic divisions of the lithosphere; the origin of the early and late crust, lithosphere and the Earth as a cosmic (with an estimated age of more than 4.6 billion years) and planetary (from the catarchean time) body; the nature of the central ring geological structures; the genesis of the largest ore and combustible (oil, gas) deposits; the emergence of pre-life. He was the first to develop: petrological and genetic models of real petrographic (plateau-basalt and granite) geospheric layers of the Phanerozoic crust and eclogite-granulite subshells of the Early Precambrian crust, patterns of composition, structure and formation mechanism of the latter indicate the primary metamagmatic nature of the lower crust (protocor); hot-melt model of protolithosphere and ProtoEarth in the catharic; and finally, the general model of the initially “hyper-hot” PraZemlya of an older than 4.6 billion years old age, including the model of the completely melt ProtoZemly in the catarchea as a special case. In evolutionary terms, the Earth is represented by paragenesis of variously rhythmically crystallized-stratified thick refractory geospheres and thin low-melting, residual fluid-ore-magmatic asthenospheres or “critical”, auto-diafluorite zones in its radial section. From the created models, as natural consequences, certain features of the model of the origin and forecasting of the deposits of (super) giants of metal, nonmetallic and combustible minerals follow, and from the latter - the specifics of the appearance of endemic pre-life on ProtoZemly, born simultaneously with the ores of the largest mineralogenic provinces. Kuznetsov A.A. - One of the developers of the system-geological method - the main tool for studying natural bodies and revealing their essence by applying the laws and principles of the general theory of systems as a branch of cybernetics. It was on this methodological basis that he obtained fundamental (model, type of "know-how") solutions to the above-mentioned priority problems of earth sciences. The system-geological method requires the establishment of systemic emergent features of the studied objects and includes geological-geometric modeling of geological bodies, phenomena and tectono-magmatic processes of various complexity levels as an obligatory stage of research. The solutions to problems developed by him are laid in the foundation of a new scientific direction - systemic geology - an integrated system of geological knowledge based on a general theory of systems that translates traditional, classical, geology of the 19th and 20th centuries to a qualitatively new level of innovative deterministic geology of the 21st century and, thereby, bringing it together with "exact" sciences. The model of the “hyper-hot” Earth is in agreement with the theory of the super-hot and super-dense state of the initial material of the Universe G. Gamov and V. A. Hambartsumyan, proposed in the 1940-60s. The geobiogenetic model of the initial abiogenic synthesis of prelife on ProtoZemle may serve as the first chapter of biogeochemistry V.I. Vernadsky and the real cosmoplanetogeological basis of the biochemical theory of A.I. Oparina (1924, 1936) the emergence of living. Teaching V.I. Vernadsky on the nature and relationship of geological, biological and physical space-time is considered in the light of the latest achievements of physics and cosmology at the turn of the 20th and 21st centuries [1–6 and others]. He is credited with the discovery of a new, geochemical, platinum-palladium-bearing province on the territory of Russia (Anabar shield) [7].

Marked with the sign "Resident of the besieged Leningrad."

He is the author of 150 published works, including six books.

1. Kuznetsov A.A. Some regularities of trap petrogenesis (on the example of certain regions of the northwestern part of the Siberian platform). Abstract dis. ... cand. geological and mineralogical sciences. L .: Tipogr. No. 6B, 1967) ^[1] .
2. Kuznetsov A.A. Tectonic-magmatic process (geometric modeling). L .: Nedra, 1977.

3. Kuznetsov A.A. Magmatogenic nature of the Earth and geological consequences (systematic approach). L .: VSEGEI, 1992. 4. Kuznetsov A.A. Modern geological technologies (know-how developments) as applied to geological mapping, mapping and forecasting of mineral deposits. St. Petersburg: Publishing House of St. Petersburg University, 1998. 5. Kuznetsov A.A. The fluid-magmatogenic nature of the Earth, its geospheric crystalline layers (subshells), giant deposits and pre-life. St. Petersburg: Publishing House of St. Petersburg University, 2004. 6. Kuznetsov A.A. The "hyper-hot" nature of the Earth and geological consequences (problems of naphtha equipoitagenesis). SPb .: The first academic typogr. “Science”, 2014. 7. Kuznetsov A.A. Geological and mineralogical model of the Anabar shield. M .: Geoinformmark, 2001.