Native lead in the rocks of deep-lying petroliferous complexes
DOI:
https://doi.org/10.15407/dopovidi2021.03.064Keywords:
native lead, reservoir of oil and gas, thermal waters, metalliferous fluidsAbstract
The presence of native-lead aggregated particles within the secondary pores (cavities) and (micro) fractures is established as a result of the electronic-microscope (with energy dispersion) analysis of deep-lying oil-and-gas reservoir rocks. Their granular (sinter-collomorphic), lamellar and microinjection morphologic types are distinguished Native lead particles (similar to other native metals) may be considered as the tracks of superdeep (mantle) reduced fluids. An additional point to emphasize is connected with its high plasticity owing which the lead particles may serve as tectonophysics indicators of a microstress distribution within deep-lying reservoir rocks.
Downloads
References
Kostov, I. (1971). Mineralogy. Moscow: Mir (in Russian).
Shtrubel, G. & Zimmer, Z. (1987). Mineralogical dictionary. Moscow: Nedra (in Russian).
Lazarenko, E. K., Panov, B. S. & Pavlishin, V. I. (1975). The mineralogy of the Donetsk Basin. Pt. 2. Kyiv: Naukova Dumka (in Russian).
Novgorodova, M. I. (1983). Native metals in hydrothermal ores. Moscow: Nauka (in Russian).
Vinogradov, A. P. (1956). Regularities of the distribution of chemical elements in the earth's crust. Geokhimiya, No. 1., рр. 6-52 (in Russian).
Lebedev, L. M. & Nikitina, L. B. (1983). Cheleken ore-forming system. Moscow: Nauka (in Russian).
Flerov, G. N., Korotkin, Yu. S., Ter-Akopyan, G. M., Zvara, I., Oganesian, Yu. Ts., Popeko, A. G., Chuburkov, Yu. T., Chelnokov, L. P., Maslov, O. D., Smirnov, V. I. & Gerstenberger, R. (1978). The results of searches for super heavy elements in the geothermal waters of the Cheleken peninsula. Dubna, OIYuI (in Russian). 8. G.N. Flerov Laboratory of Nuclear Reactions. (2006). Dubna: OIYuI (in Russian). Retrieved from http://theor.jinr.ru/people/Sissakian/CV/public/2006/dubna/Dubna273-337.pdf
Korotkin, Yu. S., Ter-Akopyan, G. M., Popeko, A. G., Drobina, T.P. & Zhuravleva, E.L. (1982). Chemical concentration of a new natural spontaneously fissile nucleid from solutions with a low salt background.Dubna, OIYuI (in Russian).
Nikitin, A. I. (1970). New transuran is found in nature. Nauka i zhizn, No. 2, рр. 102-107 (in Russian).
Lukin, A. Yu. & Shestopalov, V. M. (2020). Ferrosilicide as indicator of mineral composition of the Earth mantle? Geophys. J., 42., No. 5, рр. 3-15 (in Russian). https://doi.org/10.24028/gzh.0203-3100.v42i5.2020.215069
https://doi.org/10.24028/gzh.0203-3100.v42i5.2020.215069
Lukin, A. Yu. (2009). Native-metallic micro- and nano-inclusions in formations of oil and gas-bearing basins as tracers of superdeep fluids. Geophys. J., 31, No. 2, рр. 61-92 (in Russian).
Lukin, A. Yu. (1989). Genetical types of secondary alteration and oil-gas accumulation in aulacogenic basins: Preprint/AS USSR. Institute of Geol. Sciences. Kyiv (in Russian).
Lukin, A. Yu. (2000). Injection of deep hydrocarbon-polymineral matter in deep-seated rocks of oil and gas basins: nature, applied and epistemological significance. Geol. J., No. 2, рр. 7-21 (in Russian).
Shestopalov, V. M., Lukin, A. Yu., Zgonnik, V. A., Makarenko, L. N., Larin, N. V. & Boguslavsky, A. S. (2018). Essays on Earth degassing. Kyiv. Nauch.-Inzh. Centr Radiogidrogeojekol. Poligon. Issled., IGN NAN Ukrainy (in Russian).
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2021 Reports of the National Academy of Sciences of Ukraine
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
