Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic inversion of rift-like structure

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dc.citation.epage65
dc.citation.issue2(31)
dc.citation.journalTitleГеодинаміка
dc.citation.spage53
dc.contributor.affiliationУкраїнський науково-дослідний інститут природних газів
dc.contributor.affiliationХарківський національний університет ім. В. Н. Каразіна
dc.contributor.affiliationUkrainian Research Institute of Natural Gases
dc.contributor.affiliationKarazin Kharkiv National University
dc.contributor.authorБартащук, Олексій
dc.contributor.authorСуярко, Василь
dc.contributor.authorBartashchuk, Oleksii
dc.contributor.authorSuyarko, Vasyl
dc.coverage.placenameЛьвів
dc.coverage.placenameLviv
dc.date.accessioned2023-07-03T07:56:10Z
dc.date.available2023-07-03T07:56:10Z
dc.date.created2021-02-23
dc.date.issued2021-02-23
dc.description.abstractДосліджено системну організацію інверсійних деформацій Дніпровсько-Донецької западини та Західно-Донецького грабена. На підставі структурно-кінематичного аналізу деформаційних структур, ідентифікованих у складчастих поверхах осадового чохла, з урахуванням попередніх моделей інвер- сійного структуроформування, зроблено спробу створити оригінальну модель тектонічної інверсії рифтогенної структури. Тектонічна інверсія Дніпровсько-Донецької западини та Донбасу розпочалася в пізньогерцинську епоху в геодинамічному режимі загальноплитної колізії. Тектонофізичний аналіз інверсійних деформацій свідчить, що складчастість у западині та лінійні анти- та синформи Донбасу формувалися під впливом природного механізму поздовжнього вигину внаслідок колізійного жолоб- лення горизонтів у геодинамічному режимі транспресії. В пізньому мезозої – кайнозої інверсія про- довжувалася у полі правобічних горизонтально-зсувних деформацій із перемінною стискальною складо- вою. Цим режимом зумовлено формування складчастих тектонічних покривів та їх насування з боку Донбасу на герцинські неоавтохтонні утворення Західно-Донецького грабена та слабодислокований синеклізний автохтон південного сходу западини. Через тиск тектонічного штампа складчастого Донбасу сформувався Західно-Донецький тектонічний сегмент, який ідентифіковано структурним ороклином поперечного висування осадових геомас. У фронті та осьовій зоні тектонічного ороклину утворилися геодинамічні смуги нагнітання та витискання геомас, де формувалися великі лінійні складчасті зони. У форланді ороклину вторгнення, на закінченнях магістральних насувів, що слугували “тектонічними рейками” вторгнення геомас алохтону в рифтогенну структуру, в западині сформувалося передове лускате віяло стискання. У хінтерланді – тилу ороклину, в Західному Донбасі на герцинському неоав- тохтоні залягає коріння складчастих покривів насування, яким сформовані тектонічні сутури. На підставі вивчення системної організації колізійних деформацій Західно-Донецького грабену принципово роз- роблено модель структурно-кінематичної еволюції земної кори Дніпровсько-Донецької западини на колізійному етапі. Згідно із нею, тектонічна інверсія рифтогенної структури на території Західно- Донецького грабену зумовлена вторгненням під тиском тектонічного штампа складчастого Донбасу тектонічного сегмента вклинювання дислокованих осадових геомас із формуванням Західно-Донецької покривно-складчастої тектонічної області. Дані щодо системної організації інверсійних перебудов рифтогенної структури покладено в основу оригінальної геодинамічної моделі тектонічної інверсії Дніпровсько-Донецької западини, яка може бути використана для вдосконалення схем регіонального тектонічного та нафтогазо-геологічного районування.
dc.description.abstractThe article studies the system organization of inversion tectonic deformations of the Dnieper-Donetsk Basin which covered the territory of the Western Donetsk Graben. The research uses the kinematic and structuralparagenetic analysis of inversion structural transformation of the folded floors of the sedimentary cover of the Graben. The original model of tectonic inversion of the Dnieper-Donets Basin was completed from the previous models. The tectonic inversion of the Dnieper-Donets Paleorift rift-like structures began at the late Hercynian stage in the geodynamic environment of the territory of the Eastern European Platform general collision. Tectonophysical analysis shows that the inversion folding was formed by the mechanism of sedimentary horizons longitudinal bending in the environment of the interference of the intraplate submeridional collision compression and the regional strike-slip stress field. At the Mesozoic-Cenozoic stage, tectonic inversion continued in the field of right-hand strike-slip deformations with a variable compressive component. This caused the formation of folded covers of tectonic plates and scales in the uplift-thrust mode. They, Hercynian neoautochthonous formations and further the weakly located syneclise autochthon of the South-east of the Basin. The pressure of the “tectonic stamp” geoblock of the Donetsk Foldbelt contributed to the formation of the Segment body of geomass Tectonic Wedging. It was diagnosed with a structural orocline of transverse extension of the sliding type. Large linear throw-folded zones were formed within geodynamic bands of injection and displacement of geomass along the front of the orocline. The tectonic compression fan, characteristic of geodynamic compression zones, was formed in the foreland of the orocline, on the ends of the main thrusts. They served as “tectonic rails”of the allochthon invasion within the rift-like structure. There are the transverse zones of tectonic sutures formed on the roots of the folding covers of the Hercynian neo-autochthon thrusting, which are located in the hinterland of the orocline in the Foldbelt Western slope. The study completed an original kinematic model of tectonic inversion of the transition zone between the Dnieper-Donets Basin and Donets Foldbelt. According to the model, the pressure of the “tectonic stamp” geoblock initiated the invasion of the Segment of Tectonic Wedging which consists of the intensively dislocated allochthonous geomass. The Segment destroyed the rift-like structure and formed the Western Donetsk Cover-Folded Region in the Southeastern part of the Basin. The system organization model of inversion complications of the rift-like structure in the territory of the Western Donetsk Graben will allow to improve the regional geological schemes of tectonic oil and gas zoning.
dc.format.extent53-65
dc.format.pages13
dc.identifier.citationBartashchuk O. Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic inversion of rift-like structure / Oleksii Bartashchuk, Vasyl Suyarko // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2021. — No 2(31). — P. 53–65.
dc.identifier.citationenBartashchuk O. Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic inversion of rift-like structure / Oleksii Bartashchuk, Vasyl Suyarko // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2021. — No 2(31). — P. 53–65.
dc.identifier.doidoi.org/10.23939/jgd2021.02.053
dc.identifier.urihttps://ena.lpnu.ua/handle/ntb/59359
dc.language.isoen
dc.publisherВидавництво Львівської політехніки
dc.publisherLviv Politechnic Publishing House
dc.relation.ispartofГеодинаміка, 2(31), 2021
dc.relation.ispartofGeodynamics, 2(31), 2021
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dc.relation.referencesentectonic inversion. Geology and geochemistry of
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dc.relation.referencesenUkrainian).
dc.relation.referencesenBartaschuk, O. V., (2020). Tectonic inversion of the
dc.relation.referencesenDnieper-Donetsk depression. Part 1. Collision
dc.relation.referencesentectonics of the Western Donetsk graben. Bull. of
dc.relation.referencesenV. N. Karazin Kharkiv National University, series –
dc.relation.referencesen"Geology. Geography. Ecology", 52, 10–23 (in
dc.relation.referencesenUkrainian). https://doi.org/10.26565/2410-7360-2020-53-01
dc.relation.referencesenBartashchuk, O., & Suyarko, V. (2020). Geodynamics
dc.relation.referencesenof formation of the transition zone between the
dc.relation.referencesenDnieper-Donets basin and the donbas foldbelt.
dc.relation.referencesenTectonic style of inversion deformations.
dc.relation.referencesenGeodynamics, 2(29), 51–65.
dc.relation.referencesenhttps://doi.org/10.23939/jgd2020.02.051
dc.relation.referencesenBartashchuk, O., & Suyarko, V. (2021). Geodynamics
dc.relation.referencesenof formation of the transition zone between the
dc.relation.referencesenDnieper-Donets basin and the donbas foldbelt.
dc.relation.referencesenTectonic regimes and kinematic mechanisms of
dc.relation.referenceseninversion. Geodynamics, 1(30), 25–35.
dc.relation.referencesenhttps://doi.org/10.23939/jgd2021.01.025
dc.relation.referencesenGintov, O. B. (2005). Field tectonophysics and its
dc.relation.referencesenapplication in the study of deformations of the
dc.relation.referencesenearth’s crust in Ukraine. Kiev: Phoenix, 572 (in
dc.relation.referencesenRussian).
dc.relation.referencesenGonchar, V. V. (2019). Tectonic inversion of the
dc.relation.referencesenDnieper-Donets depression and Donbass
dc.relation.referencesen(models and reconstructions). Geophys.
dc.relation.referencesenJournal, 41(5), 47–86. (in Russian).
dc.relation.referencesenhttps://doi.org/10.24028/gzh.0203-3100.v41i5.2019.184444
dc.relation.referencesenGoryaynov, S. (2004). About the Laramide
dc.relation.referencesencomplication of geological structures of Ukraine.
dc.relation.referencesenReports of the National Academy of Sciences of
dc.relation.referencesenUkraine, 12, 114–121.
dc.relation.referencesenGoryaynov, S. (1999). About Alpine complication of
dc.relation.referencesengeological structure in various re-gions of
dc.relation.referencesenUkraine. Reports of the National Academy of
dc.relation.referencesenSciences of Ukraine, 8, 106–111.
dc.relation.referencesenGoryainov, S. V., & Sklyarenko, Yu. I. (2017).
dc.relation.referencesenForecast of lithological traps of the south-east of
dc.relation.referencesenthe DDZ within the licensed areas of
dc.relation.referencesen"Shebelinkagazvydobuvannia". Part 1. Creation of
dc.relation.referencesena structural-geological basis: report on research
dc.relation.referencesen(final): No. 100 SHGV 2017-2017 (No. 34.521, 2017–2017). Ukr. Science. dosl. Inst. of Natural
dc.relation.referencesenGases. Kharkiv, 203 (in Ukrainian).
dc.relation.referencesenDudnik, V. A., & Korchemagin, V. A., (2004).
dc.relation.referencesenCimmerian stress field within the Olkhovatsko-
dc.relation.referencesenVolyntsev anticline of Donbas, its connection with
dc.relation.referencesendiscontinuous structures and magmatism.
dc.relation.referencesenGeophys. Journal, 26(4), 75–84 (in Russian).
dc.relation.referencesenKazmin, V. G., Tikhonova, N. F. (2005). Early
dc.relation.referencesenMesozoic marginal seas in Black Sea – Caucasus
dc.relation.referencesenregion: Paleotectonic reconstructions.
dc.relation.referencesenGeotectonics, 39 (5), 349–363 (in Russian).
dc.relation.referencesenKhain, V. E. (1977). Regional geotectonics. Extra-
dc.relation.referencesenAlpine Europe and Western Asia, 185–205.
dc.relation.referencesenMoscow: Nedra (in Russian).
dc.relation.referencesenKopp, M. L., Korchemagin, V. A. (2010). Cenozoic
dc.relation.referencesenstress and deformation fields of Donbas and their
dc.relation.referencesenprobable sources. Geodynamics, 1 (9), 37–49 (in
dc.relation.referencesenRussian). https://doi.org/10.23939/jgd2010.01.037
dc.relation.referencesenKopp, M., Kolesnichenko, A., Mostryukov, A.,
dc.relation.referencesenVasilev, N. (2017). Reconstruction of Cenozoic
dc.relation.referencesenstress and deformations in the eastern East
dc.relation.referencesenEuropean platform with its regional and practical
dc.relation.referencesenapplication. Geodynamics, (23), 46–67 (in
dc.relation.referencesenRussian). https://doi.org/10.23939/jgd2017.02.046
dc.relation.referencesenKopp, M. (1991). Structural patterns of within-fold
dc.relation.referencesenbelts horizontal movements. Geotectonics, 1, 21–36 (in Russian).
dc.relation.referencesenKopp, M. L (1991). The problem of space for
dc.relation.referencesendeformations arising in the shear stress field (on
dc.relation.referencesenthe example of the Mediterranean-Himalayan
dc.relation.referencesenorogenic belt). Strike-slip tectonic disturbances
dc.relation.referencesenand their role in the formation of minerals.
dc.relation.referencesenMoscow: Nauka Publ., 75–85 (in Russian).
dc.relation.referencesenKorchemagin, V. A., Ryaboshtan, Yu. S. (1987).
dc.relation.referencesenTectonics and stress fields of Donbas. Fields of
dc.relation.referencesenstresses and strains in the earth's crust. Moscow:
dc.relation.referencesenNauka, 167–170. (in Russian).
dc.relation.referencesenKorchemagin, V. A., Emets, V. S. (1987).
dc.relation.referencesenPeculiarities of the development of the tectonic
dc.relation.referencesenstructure and stress field of Donbas and the
dc.relation.referencesenEastern Azov region. Geotectonics, 3, 49–55 (in
dc.relation.referencesenRussian).
dc.relation.referencesenMap of rupture faults and main zones of lineaments of
dc.relation.referencesenthe south-west of the USSR (using space survey
dc.relation.referencesenmaterials) scale 1: 000 000, Editor N. Krylov.
dc.relation.referencesenMoscow: Ministry of Geology of the USSR, 1988, 4 (in Russian).
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dc.rights.holder© Інститут геології і геохімії горючих копалин Національної академії наук України, 2021
dc.rights.holder© Інститут геофізики ім. С. І. Субботіна Національної академії наук України, 2021
dc.rights.holder© Національний університет “Львівська політехніка”, 2021
dc.rights.holder© Bartaschuk O., Suyarko V.
dc.subjectтектонічна інверсія
dc.subjectзони колізійного стиснення
dc.subjectструктурні деформації
dc.subjectороклин поперечного висування
dc.subjectсегмент тектонічного вклинювання
dc.subjectЗахідно-Донецька покривно-складчаста область
dc.subjecttectonic inversion
dc.subjectcollision compression zones
dc.subjectstructural deformations
dc.subjectorocline of transverse extension of the sliding type
dc.subjectSegment of Tectonic Wedging of geomass
dc.subjectWestern Donetsk Cover-Folded Region
dc.subject.udc551.24.548
dc.subject.udc242.7
dc.subject.udc248 (477)
dc.titleGeodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic inversion of rift-like structure
dc.title.alternativeГеодинаміка формування перехідної зони між Дніпровсько-Донецькою западиною і Донецькою складчастою спорудою. Тектонічна інверсія рифтогенної структури
dc.typeArticle

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