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Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia)

Šajnović, Aleksandra; Simić, Vladimir; Jovančićević, Branimir; Cvetković, Olga; Dimitrijevic, Radovan; Grubin, Nenad

(Wiley-Blackwell Publishing, Inc, Malden, 2008)

TY  - JOUR
AU  - Šajnović, Aleksandra
AU  - Simić, Vladimir
AU  - Jovančićević, Branimir
AU  - Cvetković, Olga
AU  - Dimitrijevic, Radovan
AU  - Grubin, Nenad
PY  - 2008
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/871
AB  - Sediments of the western part of the Valjevo-Mionica basin (Serbia) were examined both geochemically and mineralogically to explain, on the basis of their sedimentological characteristics, the causes of changes in their qualitative and quantitative composition. A total of 62 samples obtained from the drillhole at depths up to 400 m was investigated. Using correlation of the obtained data, six geochemical zones were defined, two of which being specially distinguished by their mineralogical, geochemical and sedimentological characteristics. The first one, upper zone A, consists of banded marlstones interbedded with clay and oil shales and is characterized by presence of analcite and searlesite. These minerals and very high contents of Na(2)O indicate sedimentation in alkaline conditions with increased salinity in and climate. That provided pronounced water stratification, as well as higher bioproductivity in the basin and sedimentary organic matter preservation. Therefore, the zone A sediments are characterized by high organic matter contents of the type which provides good potential for production of liquid hydrocarbons. Another specific zone, zone F, contains sediments with very high MgO, K(2)O and Li concentrations. Their geochemical correlation, as well as almost complete absence of illite in this zone, indicates the presence of interstratified clay mineral type illite-saponite (lithium-bearing Mg-smectite).
PB  - Wiley-Blackwell Publishing, Inc, Malden
T2  - Acta Geologica Sinica. English Edition
T1  - Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia)
VL  - 82
IS  - 6
SP  - 1201
EP  - 1212
UR  - https://hdl.handle.net/21.15107/rcub_cherry_871
ER  - 
@article{
author = "Šajnović, Aleksandra and Simić, Vladimir and Jovančićević, Branimir and Cvetković, Olga and Dimitrijevic, Radovan and Grubin, Nenad",
year = "2008",
abstract = "Sediments of the western part of the Valjevo-Mionica basin (Serbia) were examined both geochemically and mineralogically to explain, on the basis of their sedimentological characteristics, the causes of changes in their qualitative and quantitative composition. A total of 62 samples obtained from the drillhole at depths up to 400 m was investigated. Using correlation of the obtained data, six geochemical zones were defined, two of which being specially distinguished by their mineralogical, geochemical and sedimentological characteristics. The first one, upper zone A, consists of banded marlstones interbedded with clay and oil shales and is characterized by presence of analcite and searlesite. These minerals and very high contents of Na(2)O indicate sedimentation in alkaline conditions with increased salinity in and climate. That provided pronounced water stratification, as well as higher bioproductivity in the basin and sedimentary organic matter preservation. Therefore, the zone A sediments are characterized by high organic matter contents of the type which provides good potential for production of liquid hydrocarbons. Another specific zone, zone F, contains sediments with very high MgO, K(2)O and Li concentrations. Their geochemical correlation, as well as almost complete absence of illite in this zone, indicates the presence of interstratified clay mineral type illite-saponite (lithium-bearing Mg-smectite).",
publisher = "Wiley-Blackwell Publishing, Inc, Malden",
journal = "Acta Geologica Sinica. English Edition",
title = "Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia)",
volume = "82",
number = "6",
pages = "1201-1212",
url = "https://hdl.handle.net/21.15107/rcub_cherry_871"
}
Šajnović, A., Simić, V., Jovančićević, B., Cvetković, O., Dimitrijevic, R.,& Grubin, N.. (2008). Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia). in Acta Geologica Sinica. English Edition
Wiley-Blackwell Publishing, Inc, Malden., 82(6), 1201-1212.
https://hdl.handle.net/21.15107/rcub_cherry_871
Šajnović A, Simić V, Jovančićević B, Cvetković O, Dimitrijevic R, Grubin N. Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia). in Acta Geologica Sinica. English Edition. 2008;82(6):1201-1212.
https://hdl.handle.net/21.15107/rcub_cherry_871 .
Šajnović, Aleksandra, Simić, Vladimir, Jovančićević, Branimir, Cvetković, Olga, Dimitrijevic, Radovan, Grubin, Nenad, "Sedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia)" in Acta Geologica Sinica. English Edition, 82, no. 6 (2008):1201-1212,
https://hdl.handle.net/21.15107/rcub_cherry_871 .
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