Carpathian Foredeep Basin (Poland and Ukraine)&lt;subtitle&gt;Its Sedimentary, Structural, and Geodynamic Evolution&lt;/subtitle&gt;

Oszczypko, Nestor; Krzywiec, Piotr; Popadyuk, I. V.; Peryt, Tadeusz Marek

doi:10.1306/985612m843072

Cited by 103 publications

(162 citation statements)

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“…Ac cord ing to seis mic, magnetotelluric and bore hole data (Oszczypko et al, 2006), the Carpathian Foredeep is asym metri cal as a whole, with an ero sional bound ary in the north and a tec tonic bound ary to the south. It is filled in with pre dom i nantly clastic strata of Mio cene age.…”

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 80%

“…The molasse de pos its un der lain by the base ment of the East Eu ro pean Plat form are over lain by Perm ian-Me so zoic ter res trial and shelf strata and lo cally by Paleogene de pos its. The plat form base ment with the Mio cene molasse dips south wards be neath the Outer Carpathian units (Oszczypko et al, 2006). The Early to Mid dle Mio cene Carpathian Foredeep de vel oped as a peripherical fore land basin re lated to the mov ing Carpathian front.…”

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 97%

“…The Carpathian Foredeep is a large sed i men tary ba sin devel oped on the Carpathian front from the Dan ube River in Austria to the Iron Gates in Ro ma nia (Oszczypko et al, 2006). The fore land ba sin de vel oped as a re sult of Carpathian front movement to wards north dur ing Early to Mid dle Mio cene.…”

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 99%

“…The fore land ba sin de vel oped as a re sult of Carpathian front movement to wards north dur ing Early to Mid dle Mio cene. The in ner part of the Carpathian Foredeep is locateed be neath the Carpathian nappes whereas the outer one is placed in front of the orogen (Ney et al, 1974;Oszczypko et al, 2006).…”

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 99%

“…Over one hun dred sam ples of siliciclastic rock were ex am ined, the re sults be ing pre sented both in ear lier works of the au thors and in the pres ent pa per. These rocks are un der lain by the evaporitic suc ces sion of the Mid dle Mio cene ba sin (Oszczypko et al, 2006;Peryt, 2006). Ear lier re sults ob tained for the Mid dle Mio cene sand stones from bore holes in the Tarnogród area (Maliszewska et al, 2001a) have been used for com par i son and dis cus sion.…”

Section: Introductionmentioning

confidence: 99%

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Characteristics of diagenesis, isotopic relations and reservoir properties of the Middle Miocene sandstones in the Carpathian Foredeep (Poland and Ukraine)

Jarmołowicz-Szulc

Kozłowska

Kuberska

2015

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1 Pol ish Geo log i cal In sti tute -Na tional Re search In sti tute, Rakowiecka 4, 00-975 Warszawa, Po land Jarmo³owicz-Szulc, K., Koz³owska, A., Kuberska, M., 2015. Char ac ter is tics of diagenesis, iso to pic re la tions and res er voir prop er ties of the Mid dle Mio cene sand stones in the Carpathian Foredeep (Po land and Ukraine). Geo log i cal Quar terly, 59 (4): 750-761, doi: 10.7306/gq.1261The Up per Badenian and Sarmatian sand stones rec og nized from bore holes in south east ern Po land and west ern Ukraine are very fine to me dium-grained subarkosic and sublithic arenites and wackes. The de pos its un der went diagenesis well below 100°C, and their evo lu tion ary path ways of diagenetic and re lated res er voir prop er ties rep re sent eo-and mesodiagenesis. Eodiagenesis here com prised me chan i cal com pac tion, de vel op ment of chlorite, microcrystalline cal cite, py rite, sid er ite, kaolinite and quartz, and dis so lu tion of feld spar and mica grains. Mesodiagenesis in cluded quartz and K-feldspar overgrowths, albitisation, crystallisation of do lo mite and an ker ite and coarsely crys tal line cal cite, dis so lu tion of feld spar grains and car bon ate ce ment, and illite growth. The iso to pic data of d 18 O VPDB of car bon ate ce ments sug gest their crys tal li sation from porewater which is a mix ture of ma rine and me te oric wa ters. The d 13 C VPDB val ues sug gest der i va tion of car bon from mi cro bial methanogenesis of or ganic mat ter. The 87 Sr/ 86 Sr val ues in coarsely crys tal line cal cite are higher than those of Badenian sea wa ter. The ra dio genic stron tium may have been sup plied dur ing diagenesis by me te oric wa ters drain ing the con ti nen tal area. The Mid dle Mio cene sand stones show better fil tra tion abil i ties (good and very good) in the west ern part of the study area (Po land) than in the east. Pri mary inter gra nu lar po ros ity is more fre quent than sec ond ary intragranular and intercrystalline po ros i ties.The pri mary po ros ity was di min ished due to com pac tion and ce men ta tion from west to east. Some in crease in po ros ity was caused by dis so lu tion of de tri tal grains and by de cay of soft parts of or gan isms.

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Section: Geological Setting and Depositional Environmentsmentioning

confidence: 80%

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 97%

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 99%

Section: Geological Setting and Depositional Environmentsmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 3 more Smart Citations

Characteristics of diagenesis, isotopic relations and reservoir properties of the Middle Miocene sandstones in the Carpathian Foredeep (Poland and Ukraine)

Jarmołowicz-Szulc

Kozłowska

Kuberska

2015

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Exhumation history of the Tatry Mountains, Western Carpathians, constrained by low‐temperature thermochronology

Śmigielski¹,

Sinclair

Stuart

et al. 2016

Tectonics

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This study tests alternative models for the growth of the Tatry Mountains (Central Western Carpathians) by the application of low-temperature thermochronology. Zircon (U + Th)/He ages from the north of the range are mostly between 48 and 37 Ma and indicate cooling prior to the onset of fore-arc sedimentation in the region (42-39 Ma). In contrast, zircon (U + Th)/He ages in the south of the range are around 22 Ma. Apatite fission track ages across the sampled sites range from 20 to 15 Ma. Apatite (U + Th)/He ages range from 18 to 14 Ma with little variation with elevation or horizontal location. Based on thermal modeling and tectonic reconstructions, these Miocene ages are interpreted as cooling in the hanging wall of a northward dipping thrust ramp in the current location of the sub-Tatric fault with cooling rates of 20°C/Myr at~22-14 Ma. Modeled cooling histories require an abrupt deceleration in cooling after~14 Ma to <5°C/Myr. This is associated with termination of deformation in the Outer Carpathians and is synchronous with the transition of the Pannonian Basin from a syn-rift to a postrift stage and with termination of N-S compression in the northern part of the Central Western Carpathians. Overall, the timing of shortening and exhumation is synchronous with the formation of the Outer Carpathian orogen and so the Miocene exhumation of the Tatry records retrovergent thrusting at the northern margin of the Alcapa microplate.

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Building and exhumation of the Western Carpathians: New constraints from sequentially restored, balanced cross sections integrated with low‐temperature thermochronometry

et al. 2016

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Western Carpathian orogeny has been the subject of intense scientific debate due to the occurrence of enigmatic features, leading several authors to provide contrasting geological models. In this paper, a new interpretation for the tectonic evolution of the Western Carpathians is provided based on the following: (i) an analysis of the stratigraphy of the Mesozoic‐Tertiary successions across the thrust belt domains, (ii) a reappraisal of the stratigraphy and sedimentology of the “tectonic mélange” (i.e., the so‐called Pieniny Klippen Belt) marking the suture between the Inner and Outer Carpathians, and (iii) the construction of a series of balanced and restored cross sections, validated by 2‐D forward modeling. Our analysis provides a robust correlation of the stratigraphy from the Outer to the Inner Carpathians, independently of the occurrence of oceanic lithosphere in the area, and allows for the reinterpretation of the tectonic relationships among the Inner Carpathians, the Outer Carpathians, and the Pieniny Klippen Belt and the exhumation mechanisms affecting this orogenic belt. In order to constrain the evolution during the last 20 Ma, our model also integrates previously published and new apatite fission track and apatite (U‐Th‐Sm)/He data. These latter indicate a middle‐late Miocene exhumation of the Pieniny Klippen Belt. In this study, the recent regional uplift of the Pieniny Klippen Belt is described for the first time using a 2‐D kinematic model for the tectonic evolution of the Western Carpathians.

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Carpathian Foredeep Basin (Poland and Ukraine)<subtitle>Its Sedimentary, Structural, and Geodynamic Evolution</subtitle>

Cited by 103 publications

References 0 publications

Characteristics of diagenesis, isotopic relations and reservoir properties of the Middle Miocene sandstones in the Carpathian Foredeep (Poland and Ukraine)

Characteristics of diagenesis, isotopic relations and reservoir properties of the Middle Miocene sandstones in the Carpathian Foredeep (Poland and Ukraine)

Exhumation history of the Tatry Mountains, Western Carpathians, constrained by low‐temperature thermochronology

Building and exhumation of the Western Carpathians: New constraints from sequentially restored, balanced cross sections integrated with low‐temperature thermochronometry

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