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1.
G. V. Ovchinnikova A. B. Kuznetsov I. M. Vasil’eva I. M. Gorokhov M. T. Krupenin A. V. Maslov T. L. Turchenko 《Stratigraphy and Geological Correlation》2008,16(2):138-142
The mineral composition and U-Pb and Rb-Sr systematics of phosphorites from the Satka Formation of Lower Riphean carbonates, the Burzyan Group of Southern Urals, are studied. Phosphorites occurring as small lenses between stromatolite layers are composed largely of fluorapatite with admixture of detrital quartz, feldspars, illite, and chlorite. Phosphorite samples have been subjected to stepwise dissolution in 1 N (fraction L-1) and 2 N (fraction L-2) HCl. As is established, the maximum apatite content is characteristic of fraction L-1, while fraction L-2 is enriched in products of dolomite and sulfide dissolution and in elements leached from siliciclastic components. The Sr content in the Satka apatites (280–560 ppm) is substantially lower as compared with that in unaltered marine apatite. The 87Sr/86Sr “initial ratio in the phosphorites studied (0.71705–0.72484) and host dolomites from the lower part of the Satka Formation is significantly higher than in the Early Riphean seawater that indicates a reset of the Rb-Sr original systems in sediments. The Pb-Pb age of 1340 ± 30 Ma (MSWD = 6.4) estimated based on 7 data points characterizing fractions L-1 and L-2 is younger than the formation time of overlying Burzyan sediments, being consistent, within the error range, with date of the Mashak rifting event recorded at the Early-Middle Riphean boundary. The comparative U-Pb characteristics of two soluble fractions (L-1 and L-2) and silicate residue of phosphorites show that epigenetic redistribution of Pb and U was characteristic of the phosphorite horizon only. The initial Pb isotope composition and μ (238U/204Pb) estimated according to model by Stacey and Kramers for the early diagenetic fluids in carbonate and phosphate sediments of the Satka Formation suggest that they were in isotopic equilibrium with erosion products of the Taratash crystalline complex. 相似文献
2.
U-Th-Pb systematics of precambrian carbonate rocks: Dating of the formation and transformation of carbonate sediments 总被引:1,自引:0,他引:1
O. K. Kaurova G. V. Ovchinnikova I. M. Gorokhov 《Stratigraphy and Geological Correlation》2010,18(3):252-268
The current state in the Pb-Pb dating of the formation and epigenesis of Precambrian carbonate sediments has been reviewed.
The geochemistry of admixture elements (U, Th, Pb, Rb, Sr, Mn, and Fe) constituting carbonate minerals and the redistribution
of the elements in the course of early diagenesis and epigenesis have been considered. The advantages of choosing samples
for Pb-Pb dating on the basis of geochemical criteria similar to those applied for Sr-isotope stratigraphy and the potentialities
of applying different methods of decontamination of specimens, analyzed from surface contamination and possible epigenetic
carbonate phases, were illustrated. By the example of a series of carbonate formations, distinctions in susceptibility of
U-Pb and Rb-Sr systems of carbonate minerals to secondary transformations have been demonstrated. The prospects for using
the method of step solution allowing noncogenetic carbonate generations to be separated and thus the accuracy and reliability
of Pb-Pb dates to be upgraded were considered. 相似文献
3.
S. I. Prokopiev T. E. Ovchinnikova O. F. Vasiliev 《Izvestiya Atmospheric and Oceanic Physics》2010,46(2):256-260
To adequately describe the hydrophysical processes in water bodies with a high mineralization, it is necessary to take into
account the dependence that the thermodynamic characteristics of water have on the amount of salts contained in it. This work
investigates some widely known formulas for calculating a number of thermodynamic parameters of mineralized water. The density,
freezing temperature, specific heat of evaporation, and relative pressure of saturated vapor over the surface are considered.
The possibilities of using these formulas when modeling hydrophysical processes in water bodies with salinity in the range
of 0–250 pro mille are analyzed. It is shown that the formulas under consideration should be used when the salinity does not
exceed 100 pro mille. If the mineralization is higher, it is necessary to elaborate more suitable formulas on the basis of
an approximation of in situ data or data from handbooks. 相似文献
4.
G. V. Ovchinnikova A. B. Kuznetsov I. M. Vasil’eva I. M. Gorokhov E. F. Letnikova B. M. Gorokhovskii 《Stratigraphy and Geological Correlation》2012,20(6):516-527
The U-Pb and Pb-Pb methods were used for determining age of cap limestones from the Neoproterozoic Tsagaan Oloom Formation corresponding to the lower part of the sedimentary cover in the Dzabkahn microcontinent of Central Asia. The weighted average age value appeared to be equal to 632 ± 14 Ma (MSWD = 0.11, probability 0.74). This value allows the following assumptions: (1) the lower boundary of the Tsagaan Oloom Formation corresponds to the beginning of the Ediacaran; (2) Dzabkhan tillites are correlative with glacial sediments of the Marinoan Epoch. The low 238U/204Pb and 232Th/238U ratios observed in initial Pb sources of limestones from the Tsagaan Oloom Formation indicate that the Dzabkhan paleobasin received at its early development stages a bulk of material from eroded upper Riphean juvenile rocks. The 87Sr/86Sr ratio in fractions of Tsagaan Oloom limestones enriched with primary carbonate material and satisfying geochemical criteria of Rb-Sr systems retentivity (Mn/Sr < 0.20 and Fe/Sr < 1) varies from 0.70676 to 0.70691 and reflects this ratio in the World Ocean approximately 630 Ma ago. 相似文献
5.
G. V. Ovchinnikova A. B. Kuznetsov I. M. Vasil’eva I. M. Gorokhov M. T. Krupenin B. M. Gorokhovskii A. V. Maslov 《Doklady Earth Sciences》2013,451(2):798-802
The Pb-Pb age of phosphorite concretions of the Zigaza-Komarovo Formation, which composes the intermediate horizons of the Riphean stratotype of the South Urals, was determined in fractions resulting from the stepwise dissolution of concretions in 0.1 N, 0.5 N, and 1 N HCl. The determination of the Sr isotopic composition in phosphate fractions was favorable for rejection the fractions polluted with extraneous material. On the 207Pb/204Pb-206Pb/204Pb diagram, the isochron based on 31 points corresponds to 1330 ± 20 Ma (MSWD = 1.12), which is in agreement with the stratigraphic position of the Zigaza-Komarovo Formation. The decreased μ2 value of 9.57 for the phosphorite concretions relative to that of the average earthly lead based on the Stacey-Kramers model (9.74) is related to the rocks with an admixture of mantle lead, which occur in the run-off area of the Zigaza-Komarovo sediments. 相似文献
6.
Oparin I. D. Charikov Yu. E. Ovchinnikova E. P. Shabalin A. N. 《Geomagnetism and Aeronomy》2020,60(7):889-895
Geomagnetism and Aeronomy - We study the electron energy spectra of two powerful solar flares SOL2003-10-28T 1106:16 (GOES class X17.2) and SOL2002-07-23T 0018:16 (X4.8) analyzing the HXR and... 相似文献
7.
A. B. Kuznetsov I. M. Gorokhov G. V. Ovchinnikova V. A. Melezhik I. M. Vasil’eva B. M. Gorokhovskii G. V. Konstantinova N. N. Mel’nikov 《Lithology and Mineral Resources》2011,46(2):151-164
The Rb-Sr and U-Pb systematics have been studied in the metasedimentary carbonate rocks from the Paleoproterozoic Kuetsjarvi
Formation. Samples were taken from the borehole drilled in the northern zone of the Pechenga Greenstone Belt in the northwestern
Kola Peninsula. The carbonate section of the formation is made up of three units (from the bottom to top): (I) dolomite (68
m), (II) calcareous-dolomite (9 m), and (III) clayey calcareous (1 m) ones. Dolomites (Mg/Ca = 0.55–0.61) from the lowermost
unit I contain 70.3–111 ppm Sr. Initial 87Sr/86Sr ratio in them varies within 0.70560–0.70623 and characterizes the primary continental-lacustrine carbonate sediments. Calcareous
dolomites (Mg/Ca = 0.39–0.59) and dolomitic limestones of units II and III (Mg/Ca = 0.02–0.36) are enriched in Sr (285–745
and 550–1750 ppm, respectively). Initial 87Sr/86Sr ratios in these rocks (0.70406–0.70486 and 0.70407–0.70431, respectively) fall within the range typical of the Jatulian
seawater, which indicates that the carbonate sediments of two upper units were formed in an open marine basin. Study of dolomites
from unit I showed that the Svecofennian metamorphism more significantly affected the U-Pb systems of carbonate rocks as compared
to their Rb-Sr systems. In the 207Pb/204Pb-206Pb/204Pb diagram, most data points corresponding to the carbonate constituent of dolomites define isochron with an age of 1900 ±
25 Ma (MSWD = 0.5). The same samples define a positive correlation in the 208Pb/204Pb-206Pb/204Pb plot. Since sedimentary carbonates usually do not contain Th, this correlation points to secondary enrichment of the studied
dolomites in Th or thorogenic 208Pb. Hence, the obtained Pb-Pb dating can be regarded as the age of the Svecofennian metamorphic event. Three samples from
dolomites of unit I lack any disturbance of the initial U-Th-Pb systematics, but their trend in the 207Pb/204Pb-206Pb/204Pb diagram deviates from the 1900 Ma isochron. Based on these samples, the model U-Pb premetamorphic age of the Kuetsjarvi
carbonate sediments is 2075–2100 Ma. This interval is consistent with the age range of the Lomagundi-Jatulian event, which
was responsible for the formation of carbonate sediments with high positive δ13C values. 相似文献
8.
Geomagnetism and Aeronomy - Modern observations of solar flares in hard X-rays are carried out with a high spatial resolution of ~2–4 arcsec with the RHESSI satellite. In this way one can... 相似文献
9.
Globina V. I. Shabalin A. N. Ovchinnikova E. P. Charikov Yu. E. 《Geomagnetism and Aeronomy》2019,59(7):890-897
Geomagnetism and Aeronomy - The results of the study of quasi-periodic hard X-ray pulsations in solar flares with respect to the spatial localization of emission sources based on data from the... 相似文献
10.