№66-16
On the use of Middle Dnipro region granites in the pre-industrial period
I. Nikitenko1
1Dnipro University of Technology, Dnipro, Ukraine
Coll.res.pap.nat.min.univ. 2021, 66:165-176
https://doi.org/10.33271/crpnmu/66.165
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ABSTRACT
Purpose. To determine geological complexes of granites and granitoids of the Ukrainian Shield, which were mined on the territory of the Middle Dnipro region in antiquity, using the results of archaeological and petrographic studies. To establish the features of the use of the mineral resource base of granites and granitoids from the beginning of their exploitation to the current stage of mining development.
The methods are represented by the analysis of the results of petrographic studies of various stone artefacts made of granites and the correlation of the data obtained with information about the geology of the Ukrainian Shield and the presence of outcrops of these rocks available for extraction by ancient miners.
Findings. As a result of the analysis, it was determined that the granites and granitoids, extracted in the Middle Dnipro region and used throughout history, belong to the rocks of the Fastivskyi, Dnipropetrovskyi, Surskyi, Mokromoskovskyi, Tokivskyi, Saksahanskyi and Inhuletskyi complexes. The rocks of the Demurynskyi and Tetiivskyi complexes of granites were probably also applied. The history of use of the granites and granitoid rocks of the Middle Dnipro region continues since the Upper Paleolithic. Granites served as a material for the manufacture of tools and as the main building stone in the zone of distribution of rocks of the Ukrainian Shield. Their specialized development with the use of mining techniques originated with the emergence of megalithic constructions and stone stelae, which were created in the Middle Dnipro region up to and including the Middle Ages. In the times of Kyiv Rus, granite became one of the main types of building stone, which was applied in stone architecture. It can be affirmed that the development of many deposits that are currently under exploitation or were exploited during the 20th century began about a thousand years ago.
The originality. For the first time, a holistic characteristic of the use of granites and granite-like rocks of the Middle Dnipro region, from the Paleolithic era to the beginning of their industrial development in modern times, is given. Based on the results of petrographic analyzes, a list of intrusive-magmatic and ultrametamorphic complexes of the Ukrainian Shield is presented, which served as a source of granites as raw materials in the studied region throughout history.
Practical implementation. The research results will be used in writing scientific and educational works on the history and archaeology of Ukraine and the Middle Dnipro region.
Keywords: granites, history of mining, archaeological petrography, Middle Dnipro region.
References
- Petrun, V.F. (1969). Do pokhodzhennia mineralnoi syrovyny pam’iatnykiv III – I tysiacholittia do n.e. z baseinu richky Inhulets. Arkheolohiia, 22, 68–79.
- Stepanchuk, V., & Petrоugne, V. (2005). Raw materials as source for tracing migration: the case of Mira in Middle Dnieper area. Archaeometriai Műhely, 4, 38–45.
- Heraskova, L.S. (1991). Skulptura serednovichnykh kochovykiv stepiv Skhidnoi Yevropy. Naukova dumka.
- Pletneva, S.A. (1974). Polovetskie kamennye izvayaniya: Svod arkheologicheskikh istochnikov. (Vyp. U4-2). Nauka.
- Berezanskaya, S.S., Tsvek, E.V., Klochko, V.I., & Lyashko, S.N. (1994). Remeslo epokhi eneolita-bronzy na Ukraine. Naukova dumka.
- Nikitenko, I.S., & Kutsevol, M.L. (2016). On raw materials of Neolithic stone hoes from the Dnieper rapids area. Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu, 4, 5–12.
- Nikitenko, I.S. (2018). Osoblyvosti vykorystannia hirskykh porid u starodavnii kam’ianii plastytsi Serednoho Prydniprov’ia. Forum hirnykiv–2018: materialy mizhnarodnoi konferentsii, (NTU «Dniprovska politekhnika», m. Dnipro, 10 – 13 zhovtnia 2018 r.). (s. 218–226). Seredniak T.K
- Nikitenko, I.S., & Polin, S.V. (2016). Proiskhozhdeniestroitel'nogokamnyakrepidyipantsiryaAleksandropol'skogokurgana. Heoloho-mineralohichnyi visnyk Kryvorizkoho natsionalnoho universytetu, 1, 37–45.
- Nikitenko, I.S., Kutsevol, M.L., & Kovalenko, E.D. (2013). RezultatypetrohrafichnohodoslidzhenniakolektsiistarodavnikhzhorenzfondivDnipropetrovskohonatsionalnohoistorychnohomuzeiuim. D.I. Yavornytskoho. Zbirnyk naukovykh prats Natsionalnoho hirnychoho universytetu, 41, 11–18.
- Nikitenko, I.S., & Kutsevol, M.L. (2012). Doslidzhennia syrovyny kam’ianykh vyrobiv periodu neolitu-bronzy z kolektsii Dnipropetrovskoho natsionalnoho istorychnoho muzeiu im. D.I. Yavornytskoho. Zbirnyk naukovykh prats Natsionalnoho hirnychoho universytetu, 38, 11–19.
- Nikitenko, I.S., & Yolshyn, D.D. (2009). Rezultaty mineraloho-petrohrafichnoho doslidzhennia budivelnoho kaminnia z fundamentiv Desiatynnoi tserkvy u Kyievi. Koshtovne ta dekoratyvne kaminnia, 6, 22–27.
- Shcherbakov, I.B. (2005). PetrologiyaUkrainskogoshchita. ZUKTs.
- Yesypchuk, K.Yu., Bobrov, O.B., Stepaniuk, L.M., Shcherbak, M.P., Hlevaskyi, Ye.B., Skobeliev, V.M., Drannyk, A.S., & Heichenko, M.V. (2004). Koreliatsiina khronostratyhrafichna skhema rannoho dokembriiu Ukrainskoho shchyta (poiasniuvalna zapyska).UkrDHRI.
- Orsa, V.I. (1973). Petrolohiia hranito-hneisovoho kompleksu Serednoho Prydniprov’ia.Naukova dumka.
- Sukach, V., Kurylo, S., & Hrinchenko, O. (2016). Tonalit-trond’iemit-hranodiorytovi (TTH) asotsiatsii Serednoprydniprovskoho arkheiskoho kratonu. Visnyk Kyivskoho natsionalnoho universytetu imeni Tarasa Shevchenka. Heolohiia, 1(72), 20–27.
- Shcherbakov, Y.B., Esypchuk, K.E., & Orsa, V.Y. (1984). Hranytoydnыe formatsyy Ukraynskoho shchyta. Naukova dumka.
- Stepaniuk, L.M., Bobrov, O.B., & Zakharov, V.V. (2010). Chas formuvannia hranitoidiv saksahanskoho kompleksu. Mineralni resursy Ukrainy, 1, 21–26.
- Troshchenko, V.N. (1973). Plagiogranitnye kompleksy Krivorozhsko-Kremenchugskoy strukturno-fatsial'noy zony. Sovetskaya geologiya, 3, 116–127.
- Shcherbak, N.P., & Bartnitskiy, E.N. (1995). Repernye izotopnye daty geologicheskikh protsessov i stratigraficheskaya skhema dokembriya Ukrainskogo shchita. Geokhimiya i rudoobrazovanie, 21, 3–23.
- Usenko I.S., Esipchuk K.E., Lichak I.L., Slipchenko V.A., & Tsukanov V.A. (1975). Spravochnik po petrografii Ukrainy. Magmaticheskie i metamorficheskie porody. Naukova dumka.
- Vidergauz, L.M., Alekseev, Yu.N., & Bilichenko, E.Ya. (1964). Stroitel'nye materialy Dnepropetrovskoy oblasti. Budivelnyk.
- Semenenko, N.P. (1958). Tokovskiy granitnyy massiv. P.Ya. Antropov (Red.), Geologiya SSSR. (T. 5, s. 271–272). Gosgeoltekhizdat.
- Usenko, O.V. (2014). Usloviya formirovaniya granitoidov Srednepridneprovskoy granit-zelenokamennoy oblasti. Geofizicheskiy zhurnal, 2 (36), 57–74.
- Bezvynnyi, V.P., & Orsa, B.I. (2001). Dioryt-tonalit-plahiohranitova formatsiia Rosynskiu-Tikytskoho raionu. Perionalni heolohichni doslidzhennia v Ukraini i pytanyia stvorennia Derzhheolkarty-200 (s. 98–100).
- Stepaniuk, L.M., Yesypchuk, K.Yu., Boichenko, S.O., Skobieliev, V.M., Dovbush, T.I., & Shcherbak, D.M. (2000). Pro chas formuvannia hranitiv baseinu richok Teteriv ta Irpin. Mineralohichnyi zhurnal, 1, 115–118.
- Zalizniak L.L. (Red.). (2005). Arkheolohiia Ukrainy (Kurs lektsii). Lybid.
- Nikitenko, I.S., & Lysenko, S.D. (2014). Rezul'taty mineralogo-petrograficheskogo analiza izdeliy iz kamnya mogil'nika Malopolovetskoe-3 i poseleniya Malopolovetskoe-2A (Kievskaya oblast'). Stratum Plus, 2, 333–345.
-
Nikitenko, I., & Suprunenko, O. (2020). Results of a petrographic study of the material of the scythian stele from the poltava Museum of local lore. Collection of Research Papers of the National Mining University, 63, 134–144.
https://doi.org/10.33271/crpnmu/63.134