Abstract
Studies on the distribution of detrital rocks, reefs, and sand-to-clay rock ratios show that geological history has witnessed the gradual differentiation between subaqueous and subaerial reliefs. An increase in the height of mountains was possible due to the immersion of the asthenospheric layer and the increase in the thickness of the continental crust in general and especially in folding areas. This led to the gradual strengthening of relief contrasts and the growth of trough depths in subduction zones. A historical change in the composition of carbonate rocks, the replacement of Archean and Lower Proterozoic limestones and siderites with dolomites and magnesites in the Middle and Upper Proterozoic and then the successive displacement of the latter by limestones in the Phanerozoic suggests a change in the acid–alkali regime of water basins and a transfer from the Archean acid basins to alkali basins in the Proterozoic and partly early Paleozoic and then to neutral and weakly alkali basins in the rest of the Phanerozoic.
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References
J. Walther, Einleitung in die Geologie als historische Wissenschaft (Gustav Fischer, Iena, 1893).
A. A. Inostrantsev, Geology: A General Course, 2nd ed. (Tipografiya M.M. Stasyukevicha, St. Petersburg, 1889), Vol. 1 [in Russian].
D. V. Nalivkin, “Asian geology,” Priroda (Moscow, Russ. Fed.), No. 12, 2–13 (1964).
A. B. Ronov, Stratisphere, or The Earth’s Sedimentary Shell (A Quantitative Study) (Nauka, Moscow, 1993) [in Russian].
V. G. Kuznetsov, “Nekton-planktonogenic carbonate formations and their evolution in the Earth’s history,” Litol. Polezn. Iskop., No. 6, 589–611 (2002).
V. G. Kuznetsov, Evolution of Carbonate Accumulation in the Earth’s History (GEOS, Moscow, 2003) [in Russian].
R. Ginsburg, “The dilemma of epicontinental peritidal carbonates,” in 27th International Geological Congress: Paper Abstracts, Vol. 9: Additional (Nauka, Moscow, 1984), pp. 88–89.
Tianrui Song and Jian Gao, “Tidal sedimentary structures from Upper Precambrian rocks of the Ming Tombs District (Peking), China,” Precambrian Res., Bei**g 29, 93–107 (1985).
D. K. Patrunov, “Sedimentary types of rocks, deposition environments, and the cyclicity of the littoral complex of carbonate and carbonate–clay sediments of the Silurian and Lower Devonian,” in Silurian and Lower-Devonian Sediments of Dolgy Island (UNTs AN SSSR, Sverdlovsk, 1980), pp. 27–53 [in Russian].
A. L. Yanshin, The Evolution of Geological Processes in the Earth’s History (Nauka, Leningrad, 1988) [in Russian].
M. I. Budyko, A. B. Ronov, and A. L. Yanshin, The History of the Atmosphere (Gidrometeoizdat, Leningrad, 1985) [in Russian].
H. E. Frimmel, “Archean atmospheric evolution: Evidence from the Witwatersrand Gold Fields, South Africa,” Earth-Sci. Rev., Nos. 1–2, 1–46 (2005).
Yu. Yu. Yurk, “Sedimentary carbonates of the upper section of the Krivoi Rog series,” Dokl. Akad. Nauk SSSR, No. 3, 459–462 (1956).
O. M. Rozen, A. A. Abbyasov, V. L. Zlobin, and V. T. Safronov, “Carbonate rocks in metamorphic complexes: Paragenesis, the mineral composition of the initial deposits, deposition environments,” Geol. Razved., No. 1, 38–47 (2003).
D. Y. Sumner, “Carbonate precipitation and oxygen stratification in Late Archean seawater as deduced from facies and stratigraphy of the Gamohaan and Frisco formations, Transvaal supergroup, South Africa,” Am. J. Sci. 297, 455–487 (1997).
I. A. Bergman, V. I. Shcherbakov, and L. K. Gavrilova, “The Li/Mg ratio as a criterion of the carbonate nature of the ore matter of Precambrian chalybeate formations,” Geokhimiya, No. 1, 53–70 (1980).
I. A. Bergman, “The lithium–magnesium ratio as a criterion of the carbonate nature of the ore matter of ferruginous–siliceous formations,” Dokl. Akad. Nauk 400 (6), 782–784 (2005).
D. G. Zavarzina, “Formation of magnetite and siderite by thermophilic Fe(III)-reducing bacteria,” Paleontol. J. 38 (6), 585–589 (2004).
K. Hattori, F. A. Cempbell, and H. R. Crose, “The occurrence of sulfur isotopes in sedimentary rocks in relation to the evolution of the Precambrian atmosphere,” Geokhimiya, No. 6, 834–849 (1985).
V. I. Vernadsky, The Chemical Structure of the Earth’s Biosphere and Its Environment (Nauka, Moscow, 1965) [in Russian].
Ch. Laschet, “On the origin of cherts,” Facies, No. 4, 459–474 (1984).
H. J. Hofmann, K. Grey, and R. I. Thorpe, “Origin of 3.45 Ga coniform stromatolites in the Warrawoona Group, Western Australia,” Geol. Soc. Am. Bull. 3, 1256–1262 (1999).
W. Nijman, K. Y. de Bruijne, and M. E. Valkcring, “Growth fault control of Earth Archean cherts, barite mounds and chart-barite veins, North Pole Dome, Eastern Pilbara, Western Australia,” Precambrian Res., Nos. 3–4, 247–274 (1999).
M. Walsh, “Microfossils and possible microfossils from the Early Archean Onverwacht Group, Barberton Mountain Land, South Africa,” Precambrian Res. 54, 271–292 (1992).
F. Westall, L. Boni, and E. Guerzoni, “The experimental silicification of microoganisms,” Paleontology, No. 3, 495–528 (1995).
F. Westall, “The geochemical environment and earliest life on Earth,” in 32nd International Geological Congress, Florence, 2004. Abstracts, Part 2, p.978.
I. A. Bergman, “Whether volcanism took part in the formation of the ferrosiliceous formation of the early Precambrian,” in Types of Sedimentogenesis and Lithogenesis and Their Evolution in the Earth’s History, Vol. 1 (IGG UrO RAN, Yekaterinburg, 2008), pp. 61–63 [in Russian].
V. G. Kuznetsov, Evolution of Sedimentary Rock Formation in the Earth’s History (Nauchnyi Mir, Moscow, 2016) [in Russian].
V. Ya. Gor’kovets and M. B. Raevskaya, “Evolution of the sedimentary process in the Neoarchean History of the Baltic Shield,” in Conceptual Problems of Lithological Research in Russia, Vol. 1 (Kazan. Univ., Kazan, 2011), pp. 249–252 [in Russian].
O. M. Rozen, “Observable signs of primary sediments and conditions of early lithogenesis in the Earth’s history,” in Conceptual Problems of Lithological Research in Russia, Vol. 2 (Kazan. Univ., Kazan, 2011), pp. 173–176 [in Russian].
V. G. Kuznetsov, “The relation between the evolution of cyanophytes and the stratigraphic arrangement of magnesites,” Geol. Razved., No. 4, 30–36 (2004).
V. A. Luchinina, Extended Abstract of Doctoral Dissertation in Geology and Mineralogy (Novosibirsk, 1990).
V. A. Luchinina, “Renalcis and Epiphyton as different stages in the life cycle of calcareous algae,” Paleontol. J. 43 (4), 463–468 (2009).
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Original Russian Text © V.G. Kuznetsov, 2018, published in Vestnik Rossiiskoi Akademii Nauk, 2018, Vol. 88, No. 6, pp. 500–507.
Vitalii Germanovich Kuznetsov, Dr. Sci. (Geol.–Mineral.), is a Professor of the Gubkin Russian State University of Oil and Gas (National Research University).
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Kuznetsov, V.G. Studies on the Evolution of Sedimentary Rock Formation As a Clue to the Solution of Several General Geological Problems. Her. Russ. Acad. Sci. 88, 192–199 (2018). https://doi.org/10.1134/S1019331618030115
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DOI: https://doi.org/10.1134/S1019331618030115