Cenozoic structural evolution, thermal history, and erosion of the Ukrainian Carpathians fold-thrust belt

Nakapelyukh, M. V.; Bubniak, Іhor; Bubniak, Andriy; Jonckheere, Raymond; Ratschbacher, Lothar

doi:10.1016/j.tecto.2017.11.009

Cited by 18 publications

(13 citation statements)

References 34 publications

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“…Structural cross-sections based on mapping the surface geology of the Eastern Carpathian nappes are generally in keeping with the reflection and velocity models, suggesting a thickness of some 8-10 km of Cretaceous and younger strata in Ukraine (e.g. Shlapinsky, 2015;Nakapelyukh et al, 2018) and in northern Romania (Stefánescu andWorking Group, 1988, Schmid et al, 2008;Matenco et al, 2010).…”

Section: Sedimentary Unitssupporting

confidence: 57%

“…Matenco and Bertotti (2000) estimated about 40 km shortening to be representative for the external nappes only of the Eastern Carpathians around the same location. To the north of RomUkrSeis (about 70 km), recent work by Nakapelyukh et al (2018), in part calibrated with fission track data, suggests a much greater degree of shortening (340-390 km). In the RomUkrSeis velocity model the Carpathian nappes are stacked to a depth of about 8 km within the Carpathian sedimentary prism (overlying older sedimentary units within it) and, since this is calibrated by geological mapping and shallow reflection studies, it is consistent with the range of palinspastic estimates of Carpathian upper crustal and sedimentary layer shortening mentioned above.…”

Section: Cenozoicmentioning

confidence: 99%

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RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield

et al. 2020

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RomUkrSeis is a controlled source wide-angle reflection and refraction (WARR) profile acquired in August 2014. It is 675 km long, running roughly SW-NE from the Apuseni Mountains in Romania and the Transylvanian Basin, crossing the arc of the Eastern Carpathian orogen and terminating in the East European Craton (EEC) in SW Ukraine. Wellconstrained 2-D ray-tracing P-and partly S-wave velocity models have been constructed along the profile from 348 single-component seismic recorders and eleven shot points. The Eastern Carpathian arc formed in the Cenozoic and have obscured the pre-existing Teisseyre-Tornquist Zone (TTZ), which is a transition zone between the Precambrian EEC and continental terranes accreted to it from the southwest in the Palaeozoic. The TTZ is characterised by low-velocity through its entire crust (6.0-6.3 km/s) and a considerable width (~140 km). It is interpreted as EEC crust stretched during rifting and continental margin formation in the Neoproterozoic and early Palaeozoic. The crust of the TTZ has a structure wherein an upper body of ~40 km width comprising Outer Carpathian (V p 4.9 km/s) and Late Palaeozoic-Mesozoic (V p 5.4 km/s) units to 15 km depth lies above a wider, deeper one of inferred Neoproterozoic-early Palaeozoic strata. The crust of the Transylvanian Basin and Apuseni Mountains is relatively thin (~32 km). A high-velocity body at 4-12 km depth in this area is interpreted as a rootless fragment of an ophiolite complex exposed at the surface in this area. The lower crust beneath the Transylvanian Basin displays higher velocities than adjacent segments. Moho topography is strongly differentiated along the profile, varying from 32 to 50 km. The Moho shape, especially in the area between the Inner and Outer Carpathians, suggests a NE dip and, hence, thrusting of the Tisza-Dacia lowermost crustal and upper mantle units under the TTZ domain which, in turn, could be thrust under the cratonic (EEC) block.

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Section: Sedimentary Unitssupporting

confidence: 57%

Section: Cenozoicmentioning

confidence: 99%

RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield

et al. 2020

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“…It runs through two nappes of the Ukrainian Carpathians -Krosno and Skyba. The other two nappes through which the Stryi Rriver flows -Boryslav-Pokuttia and Sambir ones -belong to the UCF (Nakapelyukh et al, 2018). Adjacent to these structures from the east is the Bilche-Volytska zone (Outer) of the UCF, which is an autochthonous tectonic unit.…”

Section: Geological and Sedimentological Structuresmentioning

confidence: 99%

Long term hydrological and environmental monitoring of the Stryi River using remote sensing data and GIS technologies

Burshtynska¹,

Kokhan²,

Babushka³

et al. 2021

Journ. Geol., Geogr., and Geoec..

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The proposed research sets the task of conducting monitoring aimed at determining the horizontal displacements of the channel of the Stryi River the largest right-bank tributary of the Dniester River. For this purpose, the river was zoned according to morphometric and hydrological characteristics. Three parts were identified, namely highland, piedmont and lowland ones, which radically vary in the nature of the flow and the amount of the displacement. The main research purpose consists in analyzing the impact of anthropogenic factors on the hydrological regime of the Stryi River, as well as studying the effect of the Ukrainian Carpathian Foredeep (UCF) and the Stryi Deep on the mode of horizontal displacements. The research object is processes occurring within the Stryi River channel. Considering main natural factors affecting the channel’s horizontal displacements, special attention is paid to the geological and sedimentological structures located in the region where the Stryi River and its tributaries flow; among the anthropogenic factors, deforestation and the extraction of building materials from the river channel are highlighted. Topographic, geological, soil maps and satellite images of various periods uploaded into ArcGIS software allowed us to monitor displacements observed for as long as 140 years ago. To monitoring the Stryi River channel displacements, such materials as topographic maps scaled 1: 75000 (Austrian period – 1874), 1: 100000 (Polish period – 1933, Soviet period – 1990); satellite images of Sentinel-2 (2019 and 2020 (after the flood)); a map of Quaternary sediments and a soil map scaled 1: 200000 were used. The Stryi River flows between two structures, i.e. the Skybovi Carpathians and the UCF. The right-bank tributaries (Bystrytsia, Limnitsia, Stryi, etc.), which begin in the Carpathians, cross the outer and inner boundaries of the UCF and are characterized by the stable river channel in its mountainous part, multi-braided in its piedmont part, as well as perennial and significant meandering within the Pre-Carpathian region. Lithological deposits have a significant impact at the mouth of the Stryi River. According to the research study results, displacements of up to 1,350m are measured in this area. The research includes an analysis of the influence of geological and sedimentological structures on the Stryi River displacement and the nature of its flow. It has been established that deforestation in the river basin, as well as unauthorized extraction of gravel materials, creates a significant environmental problem in this region. The results of monitoring of the channel deformation processes should be taken into account when solving problems related to river channel processes, namely the construction of hydraulic structures, the design of power transmission networks crossing rivers, the development of gas pipelines, the identification of hazardous flooding zones, the determination of consequences of destruction after floods, the establishment of boundaries of water protection zones, the management of recreational activities, monitoring of border lands and the establishment of an interstate border along rivers.

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“…1). It stretches from vicinity of Tarnów in Poland through Ukraine to Romania, were it is distinguished as Tarcau Nappe (Hnylko, 2017;Nakapelyukh et al, 2018;Matenco et al, 2010;Picha & Golonka, 2006, and references therein). The Skyba Nappe constitutes the most external Carpathian unit and represents the near-coast sedimentary area.…”

Section: Outline Of Geologymentioning

confidence: 99%

Rocky forms in the Yamna Sandstone (Skyba Nappe, Outer Carpathians, Ukraine)

Waśkowska

Hnylko

Bakayeva

et al. 2019

geotour

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Interesting objects-the rocky forms and waterfall thresholds, built of Yamna Sandstone occur in the vicinity of Skole town. Beside the esthetic positive aspects related the morphological variety of the rocky forms and occurrence of the diversified weathering structures, the objects have a substantial cognitive value encompassing the lithology and sedimentological processes of the thick-bedded turbidites. The sandstone rocky forms usually occur in the groups distributed on slopes and forming so-called rocky towns. Their number and distribution allow observation of the changing structural and textural features both lateral and vertical within the 100-m thick composed profiles. The excellent degree of rocks outcropping, variety of structural and textural features and spectrum of possible observations indicates the high geotouristic potential of the investigated objects.

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Cenozoic structural evolution, thermal history, and erosion of the Ukrainian Carpathians fold-thrust belt

Cited by 18 publications

References 34 publications

RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield

RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield

Long term hydrological and environmental monitoring of the Stryi River using remote sensing data and GIS technologies

Rocky forms in the Yamna Sandstone (Skyba Nappe, Outer Carpathians, Ukraine)

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