Burial and exhumation history of the Polish Outer Carpathians: Discriminating the role of thrusting and post-thrusting extension

Andreucci, Benedetta; Castelluccio, Ada; Jankowski, Leszek; Mazzoli, Stefano; Szaniawski, Rafał; Zattin, Massımılıano

doi:10.1016/j.tecto.2013.07.030

Cited by 40 publications

(51 citation statements)

References 29 publications

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“…Their age is com pa ra ble to the results of AHe stud ies from the Outer Carpathians (cf. Mazzoli et al, 2010;Andreucci et al, 2013) and this might sug gest that these crys tals were re-de pos ited and trans ported to the Carpathian Foredeep Ba sin from the eroded Outer Carpathian thrust sheets. The sec ond group of ap a tite crys tals is char ac ter ized by an age of 11.6 ± 1.5 Ma.…”

Section: Calcareous Nannoplanktonmentioning

confidence: 96%

Structure and evolution of the Carpathian thrust front between Tarnów and Pilzno (Pogórska Wola area, southern Poland) – results of integrated analysis of seismic and borehole data

Krzywiec¹,

Oszczypko²,

Bukowski³

et al. 2014

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Seis mic data and core from the shal low car to graphic Pilzno P-7 bore hole were used to con struct a new model of the Carpathian orogenic front be tween Tarnów and Pilzno, in the Pogórska Wola area (south ern Po land). The most ex ter nal, fron tal thrust of the orogenic wedge (the Jaoeniny struc ture) was iden ti fied as a syn-depositional fault-prop a ga tion fold detached above the Up per Badenian evaporites. Its for ma tion was con trolled by the pres ence of me chan i cally weak foredeep evaporites and by the mor phol ogy of the sub-Mio cene Meso-Pa leo zoic fore land plate (Jaoeniny and Pogórska Wola palaeovalleys). The fron tal zone of the Carpathian orogenic wedge (the Skole thrust sheet and the de formed foredeep depos its of the Zg³obice thrust sheet) is char ac ter ized by sig nif i cant backthrusting of the foredeep suc ces sion to wards the south, and by the pres ence of a tri an gle zone, with strongly de formed Up per Badenian evaporites of the Wieliczka For ma tion in its core. The tri an gle zone was formed dur ing the lat est thrust ing move ments of the Carpathians. An in di ca tion of the ex istence of the tri an gle zone in the vi cin ity of Dêbica has also been pro vided by re in ter pre ta tion of the ar chive re gional geo log ical cross-sec tion. The youn gest foredeep de pos its, brought to the sur face above the backthrust, have been dated as Sarmatian (NN7 nannoplankton zone), which in di cates that the lat est thrust move ments within the fron tal Carpathian orogenic in the vi cin ity of Tarnów-Dêbica took place approx. 11-10 mil lion years ago. Thermochronological stud ies (AFT and AHe) in di cated that the foredeep suc ces sion drilled by the Pilzno P-7 bore hole has not been bur ied deeper than 1.5-2 km, which is com pat i ble with re con struc tion based on the seis mic data.

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Section: Calcareous Nannoplanktonmentioning

confidence: 96%

Structure and evolution of the Carpathian thrust front between Tarnów and Pilzno (Pogórska Wola area, southern Poland) – results of integrated analysis of seismic and borehole data

Krzywiec¹,

Oszczypko²,

Bukowski³

et al. 2014

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“…The undeformed section resulting from the sequential restoration has then been deformed forward in time (from the Early Cretaceous to the present day) in order to validate our structural interpretation and define the structure of the eroded successions. Constraints on the maximum burial and exhumation history have been obtained by thermal modeling based on low‐temperature thermochronometric data (apatite fission track and apatite and zircon (U‐Th‐Sm)/He ages) including both new (Table ) and published data [ Anczkiewicz et al ., ; Andreucci et al ., ; Zattin et al ., , and reference therein].…”

Section: Structural Modelingmentioning

confidence: 98%

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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“…AHe re sults from the sur face sam ple (~5 km SE of the Bystry area) points to 13.4 ±2.2 Ma as a cooling tem per a ture from ~60-50°C (Andreucci et al, 2013). About 10 km east of the Bystry area, the AFT cool ing age (cool ing from ~110°C) of the sur face CCPB sam ple close to the PKB is es ti mated at 12.0 ±1.7 Ma (Anczkiewicz et al, 2013).…”

Section: Fig 8 Bse Im Ages Of Tuffitementioning

confidence: 92%

“…How ever, it is im por tant to note that both re sults are based on sin gle sam ples (other sam ples from the sur veys are not located in the vi cin ity of the Bystry Stream area). Also AFT and AHe anal y sis of the flysch-like sed i ments are prob lem atic due to of ten low qual ity of the in put ma te rial (Andreucci et al, 2013).…”

Section: Fig 8 Bse Im Ages Of Tuffitementioning

confidence: 99%

New data on the age of the sedimentary infill of the Orava-Nowy Targ Basin – a case study of the Bystry Stream succession (Middle/Upper Miocene, Western Carpathians)

Wysocka

Łoziński

Śmigielski

et al. 2018

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Burial and exhumation history of the Polish Outer Carpathians: Discriminating the role of thrusting and post-thrusting extension

Cited by 40 publications

References 29 publications

Structure and evolution of the Carpathian thrust front between Tarnów and Pilzno (Pogórska Wola area, southern Poland) – results of integrated analysis of seismic and borehole data

Structure and evolution of the Carpathian thrust front between Tarnów and Pilzno (Pogórska Wola area, southern Poland) – results of integrated analysis of seismic and borehole data

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

New data on the age of the sedimentary infill of the Orava-Nowy Targ Basin – a case study of the Bystry Stream succession (Middle/Upper Miocene, Western Carpathians)

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