Academic Journal

Cosmic microspheres in the Carboniferous deposits of the Usolka section (Urals foredeep).

التفاصيل البيبلوغرافية
العنوان: Cosmic microspheres in the Carboniferous deposits of the Usolka section (Urals foredeep).
المؤلفون: Sungatullin, R.Kh., Sungatullina, G.M., Zakirov, M.I., Tsel’movich, V.A., Glukhov, M.S., Bakhtin, A.I., Osin, Yu.N., Vorob’ev, V.V.
المصدر: Russian Geology & Geophysics; Jan2017, Vol. 58 Issue 1, p59-69, 11p
مصطلحات موضوعية: SEDIMENTARY basins, CARBONIFEROUS paleogeography, PALEOCLIMATOLOGY, SOLAR system, STRATIGRAPHIC correlation, CHEMICAL elements
مصطلحات جغرافية: URAL Mountains (Russia)
مستخلص: Magnetite microspheres from the Carboniferous deposits of the Usolka reference section were studied by probe microanalysis, with comparison of the distributions of chemical elements and microspheres. The presence of microspheres in sedimentary strata is considered to be an additional factor for stratigraphic correlation between sedimentary sections. The microspheres are shown to be of cosmic nature. The Late Paleozoic paleoclimatic changes (extreme cooling) and biotic crises were caused by the periodical Solar System motion in the Galaxy, cosmic-dust fallout, and meteorite bombardments of the Earth. [ABSTRACT FROM AUTHOR]
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قاعدة البيانات: Supplemental Index
الوصف
تدمد:10687971
DOI:10.1016/j.rgg.2016.12.003