Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina)

2018
Authors
Masod Abdulqader, SannaVakanjac, Boris
Kovacević, Jovan
Naunović, Zorana

Zdjelarević, Nevena
Article (Published version)
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Stara Planina (also known as the Balkan mountain range) is known for numerous occurrences and deposits of uranium and associated radionuclides. It is also famous for its geodiversity. The geologic framework is highly complex. The mountain is situated between the latitudes of 43 degrees and 44 degrees N and the longitudes from 22 degrees 16' to 23 degrees 00' E. Uranium exploration and radioactivity testing on Stara Planina began back in 1948. Uranium has also been mined in the zone of Kalna, within the Janja granite intrusive. The naturally radioactive geologic units of Stara Planina are presented in detail in this paper. The main sources of radioactivity on Stara Planina can be classified as: 1. Granitic endogenous-syngenetic-epigenetic deposits and occurrences; 2. Metamorphogenic-syngenetic; and 3. Sedimentary, including occurrences of uranium deposition and fluctuation caused by water in different types of sedimentary rocks formed in a continental setting, which could be classified ...under epigenetic types. The area of Stara Planina with increased radioactivity (higher than 200 cps), measured by airborne gamma spectrometry, is about 380 square kilometers. The highest values of measured radioactivity and uranium grade were obtained from a sample taken from the Mezdreja uranium mine tailing dump, where Ra-226 measures 2600 +/- 100 Bq/kg and the uranium grade is from 76.54 to 77.65 ppm U. The highest uranium (and lead) concentration, among all samples, is measured in graphitic schist with high concentrations of organic (graphitic) material from the Inovska Series-99.47 ppm U and 107.69 ppm Pb. Thorium related radioactivity is the highest in granite samples from the Janja granite in the vicinity of the Mezdreja granite mine and the Gabrovnica granite mine tailing dump, and it is the same-250 +/- 10 Bq/kg for Th-232, while the thorium grade varies from 30.82 to 60.27 ppm Th. In gray siltstones with a small amount of organic material, the highest radioactivity is related to potassium-2080 +/- 90 Bq/kg for K-40.
Keywords:
geology / radioactivity / uranium / sampling / Stara PlaninaSource:
Minerals, 2018, 8, 1Publisher:
- MDPI AG
DOI: 10.3390/min8010006
ISSN: 2075-163X
WoS: 000424127500006
Scopus: 2-s2.0-85040835494
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GraFarTY - JOUR AU - Masod Abdulqader, Sanna AU - Vakanjac, Boris AU - Kovacević, Jovan AU - Naunović, Zorana AU - Zdjelarević, Nevena PY - 2018 UR - https://grafar.grf.bg.ac.rs/handle/123456789/952 AB - Stara Planina (also known as the Balkan mountain range) is known for numerous occurrences and deposits of uranium and associated radionuclides. It is also famous for its geodiversity. The geologic framework is highly complex. The mountain is situated between the latitudes of 43 degrees and 44 degrees N and the longitudes from 22 degrees 16' to 23 degrees 00' E. Uranium exploration and radioactivity testing on Stara Planina began back in 1948. Uranium has also been mined in the zone of Kalna, within the Janja granite intrusive. The naturally radioactive geologic units of Stara Planina are presented in detail in this paper. The main sources of radioactivity on Stara Planina can be classified as: 1. Granitic endogenous-syngenetic-epigenetic deposits and occurrences; 2. Metamorphogenic-syngenetic; and 3. Sedimentary, including occurrences of uranium deposition and fluctuation caused by water in different types of sedimentary rocks formed in a continental setting, which could be classified under epigenetic types. The area of Stara Planina with increased radioactivity (higher than 200 cps), measured by airborne gamma spectrometry, is about 380 square kilometers. The highest values of measured radioactivity and uranium grade were obtained from a sample taken from the Mezdreja uranium mine tailing dump, where Ra-226 measures 2600 +/- 100 Bq/kg and the uranium grade is from 76.54 to 77.65 ppm U. The highest uranium (and lead) concentration, among all samples, is measured in graphitic schist with high concentrations of organic (graphitic) material from the Inovska Series-99.47 ppm U and 107.69 ppm Pb. Thorium related radioactivity is the highest in granite samples from the Janja granite in the vicinity of the Mezdreja granite mine and the Gabrovnica granite mine tailing dump, and it is the same-250 +/- 10 Bq/kg for Th-232, while the thorium grade varies from 30.82 to 60.27 ppm Th. In gray siltstones with a small amount of organic material, the highest radioactivity is related to potassium-2080 +/- 90 Bq/kg for K-40. PB - MDPI AG T2 - Minerals T1 - Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina) IS - 1 VL - 8 DO - 10.3390/min8010006 ER -
@article{ author = "Masod Abdulqader, Sanna and Vakanjac, Boris and Kovacević, Jovan and Naunović, Zorana and Zdjelarević, Nevena", year = "2018", abstract = "Stara Planina (also known as the Balkan mountain range) is known for numerous occurrences and deposits of uranium and associated radionuclides. It is also famous for its geodiversity. The geologic framework is highly complex. The mountain is situated between the latitudes of 43 degrees and 44 degrees N and the longitudes from 22 degrees 16' to 23 degrees 00' E. Uranium exploration and radioactivity testing on Stara Planina began back in 1948. Uranium has also been mined in the zone of Kalna, within the Janja granite intrusive. The naturally radioactive geologic units of Stara Planina are presented in detail in this paper. The main sources of radioactivity on Stara Planina can be classified as: 1. Granitic endogenous-syngenetic-epigenetic deposits and occurrences; 2. Metamorphogenic-syngenetic; and 3. Sedimentary, including occurrences of uranium deposition and fluctuation caused by water in different types of sedimentary rocks formed in a continental setting, which could be classified under epigenetic types. The area of Stara Planina with increased radioactivity (higher than 200 cps), measured by airborne gamma spectrometry, is about 380 square kilometers. The highest values of measured radioactivity and uranium grade were obtained from a sample taken from the Mezdreja uranium mine tailing dump, where Ra-226 measures 2600 +/- 100 Bq/kg and the uranium grade is from 76.54 to 77.65 ppm U. The highest uranium (and lead) concentration, among all samples, is measured in graphitic schist with high concentrations of organic (graphitic) material from the Inovska Series-99.47 ppm U and 107.69 ppm Pb. Thorium related radioactivity is the highest in granite samples from the Janja granite in the vicinity of the Mezdreja granite mine and the Gabrovnica granite mine tailing dump, and it is the same-250 +/- 10 Bq/kg for Th-232, while the thorium grade varies from 30.82 to 60.27 ppm Th. In gray siltstones with a small amount of organic material, the highest radioactivity is related to potassium-2080 +/- 90 Bq/kg for K-40.", publisher = "MDPI AG", journal = "Minerals", title = "Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina)", number = "1", volume = "8", doi = "10.3390/min8010006" }
Masod Abdulqader, S., Vakanjac, B., Kovacević, J., Naunović, Z.,& Zdjelarević, N.. (2018). Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina). in Minerals MDPI AG., 8(1). https://doi.org/10.3390/min8010006
Masod Abdulqader S, Vakanjac B, Kovacević J, Naunović Z, Zdjelarević N. Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina). in Minerals. 2018;8(1). doi:10.3390/min8010006 .
Masod Abdulqader, Sanna, Vakanjac, Boris, Kovacević, Jovan, Naunović, Zorana, Zdjelarević, Nevena, "Natural Radioactivity of Intrusive-Metamorphic and Sedimentary Rocks of the Balkan Mountain Range (Serbia, Stara Planina)" in Minerals, 8, no. 1 (2018), https://doi.org/10.3390/min8010006 . .