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Geological and Mineralogical Sciences 42 Geological and Mineralogical sciences This method of geometric correlation makes it to the Present Time. The author uses this scale in possible: lectures on historical geology for students and in 1) to get information about level of investiga- a geological museum. tion of the oil fi eld structure and about construction For the description PreArchean chronology of deposit without well-drilling; of events of formation of the Earth, the Solar 2) to identify little-studied area for building of System, method representation about “continu- the qualitative model of deposit; um” [6, 4] is used. 3) to identify area for well-drilling which re- The time scale continued in area of PreGeo- quired for building of the models deposit and for logical events of the past, possible to interpret as refi nement reserves oil; “a GeoAstronomical scale” for events PreArchean 4) to ascertain the moment in chronologies of well- time down to the moment of formation of the Our drilling, which make it possible to cut material costs; Universe [8, 1]. 5) to create the algorithm an information han- Attempts of construction of a calendar PreAr- dling on computer chean time were undertaken earlier [2, 3]. References The Principle of Stenon (for the stratigraphi- cal and the geochronological scales) illustrates 1. Bukrinskiy V.A. Geometrization of depths. – М.: MSU, stratigraphical continuum (“geocontinuum”). For 2004. – 333 р. construction of “a General Scale of Stages of Geo- 2. Gubina A.I. The Geophisical methods of stratigraphical correlation. – Perm, 2010. – 201 р. Astronomical Chronology” it is offered to use of the Principle Stenon as events-and-time, not only 3. Myagkov V.F. Geochemical method of paragenic analy- sis of ore. – M.: Nedra, 1984. – 126 р. straton-and-time. 4. Trofi mov A.A. Fundamentals of mining geometry. – M.: In this case the common geochronological scale MSU, 1980. – 224 р. becomes is a part of “Common Scale of Stages of GeoAstronomical Chronology” of events at the A COMMON SCALE OF THE STAGES Universe and at the Earth. OF A GEOASTRONOMICAL Representation of events-time (chronological), CHRONOLOGY and not just only stratigraphical geocontinuum al- Ozhgibesov V.P. lows to consider Archean-Cenozoical a stage as a component of an interval of time from formation The Perm State National Research University, of the Our Universe (13,72 ± 0,12) milliard years Perm, e-mail: [email protected] [1, 7] up to «Present Time». In this case the general For the fi rst time on the basis of a “Geocontinu- geochronological scale becomes a part of “the Gen- um” and a “Geoastronomical” continuum “A Com- eral Scale of Stages of geoastronomical chronolo- mon Scale of Stages of Geoastronomical Chronol- gy”. The geoastronomical scale allows to order and ogy” is сonstructed. Is offered new Common Scale describe chronology of events from the Big Bang to of Geoastronomical Chronology from the Big Bang the Present Time (Table). A Common Scale of the Stages of a GeoAstronomical Chronology From beginning Stages GalaYear Gelion Acron Eon Era Period (in milliard years) 12 345678 23 Retrospective Qrcnt 0 Galactic Year № 1 Q 0,018 KZ N 0,023 E 0,065 22 RGY № 2 Mesozoic К 0,15 MZ J 0,20 T 0,25 21 RGY № 3 Hertsynian P 0,30 Neozoic (NZ) С 0,35 PH Phanerozoic Geozoic (GEOZ) D 0,40 PZ 20 RGY № 4 Caledonian S 0,45 O 0,50 Є 0,54 EUROPEAN JOURNAL OF NATURAL HISTORY № 2, 2016 Geological and Mineralogical sciences 43 End Table 12 345678 19 RGY № 5 Vendian ED 0,63 V CRG 0,85 TON 1,0 (BKL) 18 6–7: Baikalian RGY2 KRT (RF3) – 1,2 Baikalian 17 8–9: Baikalian RGYPR YUR (RF2) – 1,4 16 10–11: Baikalian RGY BRZ (RF1) – 1,6 15 12–13: .Late Karelian RGYProterozoic (NZ) PRt KRL2 – 1,9 14 14–17: Late Karelian RGY (KRL) KRL1 – 2,5 13 18–21: Belomorian RGY AR Early Geosyncline 2 3,15 (BLM) Stage 12 22–27: Saamian RGY(AR) AR Geozoic (GEOZ) 1 Archean Nuclearian Stage 4,2 (SMS) 11 28–29: Regolitian RGY Regolitian Regolitian Stage. 4,3 (RGL) Lunar images 10 30–31: Accrecian RGY Accretion Stage Accretsia (PRS) of meteoric bodies, 4,5 Prisconia n (ACC) forming of the Earth 9 32–36: ProtoSolarian Proto- Forming Solarin 5,6 of ProtoEarth (PRS) 8 37–43: ProtoGalaxian Forming of Pro- Proto- toSolar System, Galaxian 7,2 axian (PGL) Galaxes. Beginning Protoplanet-Gal- (PGL) Geliozoic (GELZ) de Sitter’s Epoch 7 Epoch of formation of the fi rst Stars, Galaxies; forma- from 150 millions to 12,7 tion C, O, N, Fe 1 milliard of years 6 Epoch of formation of the fi rst atoms. Universe is fi lled 380000 years to 13,55 H, He, relic radiation of H on wave 21 sm. Stars are absent 150 millions of years 5 Epoch of beginning of forming He, deuterium, Li-7 (20 min) 3 min – 380000 years 13,70 4 Fridman’s Epoch of expansion of Our Universe; forma- 10–34 s – 3 min 13,70 tions of protons and neutrons 3 Epoch of beginning of fast expansion of Our Universe 10–43 s – l0–34 s 13,70 2 Planck’s Epoch. The fi rst instants of formation of Our from 0 to 10–43 s 13,70 Uni verse, birth of particles 1 Epoch of Singularity. The Big Bang (13,72 ± 0,12) 0 (the Beginning (13,72 ± 0,12) milliard years in the past of Histoiy of Our milliard of years Universe) Duration of the «events» located on a scale of scales PreCambrian, the analysis of cyclicity and periodicity of chronology is not criterion of ranks for the “stages” of events). – Petrozavodsk. 1997. – 93 р. geoastronomical chronology. Attributes of division of 4. Ozhgibesov V.P. General Scale of Geological time and a scale of stages, are defi ned by qualitative specifi city of a events-time GeoContinuum // Geology and minerals of the Western Urals Mountains: Materials of regional conf. (Perm events at the Earth and at the Universe [1, 5]. Duration Univ., May, 17–18th 2005). – Perm: Publishing House Perm. of a stage is not criterion of the size of division’s rank. 2005. – P. 25–28. Criterion of allocation of a separate stage is its qualita- 5. Sobotovich E.V. Isotope cosmohemistry. – M., 1974. – 208 р. tive attributes and specifi city of corresponding events. 6. The philosophical encyclopedic dictionary. – М., 1983. – 839 р. For example: three minutes of Fridman’s Epoch and 7. Hinshaw G., Weiland J.L., Hill R.S., Odegard N., Larson D., 50 millions of years for the Period of Paleozoic. Bennett C.L., Dunkley J., Gold B., Greason M.R., Jarosik N., References Komatsu E.. Nolta M. R, Page L., Spergel D.N., Wollack E., Halpern M., Kogut A., Limon M., Meyer S.S., Tucker G.S. 1. Kaku Michio. The parallel worlds. М.: Publishing House and Wright E.L. Five-Year Wilkinson Microwave Anisotropy “Sofi a”, 2008. – 416 р. Probe Observations: Data Processing, Sky Maps, and Basic Re- 2. Kulikova V.V., Kulikov V.S. A Galactic Calendar of His- sults // The Astrophysical Journal Supplement Series. – 2009. – tory of the Earth. – Petrozavodsk: the Karelian Center of the Vol. 180, № 2. – P. 225–245. Russian Academy of Science, 2000. – 14 р. 8. A Geologic Time Scale 2004 / by F.M. Gradstein, 3. Kulikova V.V., Kulikov V.S. Universal a Galactic Chron- J.G. Ogg, A.G. Smith et. al. // Cambrige University ometric Scale (Experience of comparison of world and regional Press. – 2004. EUROPEAN JOURNAL OF NATURAL HISTORY № 2, 2016.
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