GEOPLANET

Szkoła doktorska

Uprzejmie zapraszamy do zapoznania się z ofertą studiów III stopnia w szkole Geoplanet współprowadzonej przez ING PAN.

Więcej informacji

Instytut Nauk Geologicznych
Polskiej Akademii Nauk

Instytut Nauk Geologicznych Polskiej Akademii Nauk należy do Wydziału III - Nauk Ścisłych i Nauk o Ziemi PAN.

ING PAN (rok założenia 1956) jest instytutem naukowym specjalizującym się w badaniach wieku skał i minerałów oraz ich genezy, odtwarzaniu ewolucji orogenów, rekonstrukcji środowiska geologicznego ze szczególnym uwzględnieniem metod geochemii izotopów, mineralogii, petrologii, sedymentologii, tektoniki, stratygrafii i hydrogeologii oraz paleontologii. Celem naszych badań jest lepsze zrozumienie geosytemu i wykorzystanie tej wiedzy dla potrzeb nowoczesnego społeczeństwa.

Siedzibą ING PAN jest Warszawa a na cały instytut składają się zespoły badawcze i aparatura skupione w trzech badawczych ośrodkach: 
w Krakowie, w Warszawie i we Wrocławiu.

Nasze zespoły badawcze

Projekty i partnerstwo

Ostatnie publikacje

AutorzyStanisław Mazur, Waldemar Jóźwiak, Krzysztof Nowożyński, Szymon Oryński
Rok2024
TytułMagnetotelluric evidence for long-lasting crustal memory in an intraplate setting – the Grójec Fault and Mid-Polish Trough in central Poland
CzasopismoTectonophysics, 2024, 230213
DOIhttps://doi.org/10.1016/j.tecto.2024.230213

The Grójec Fault (GF) is of significant interest due to its orientation perpendicular to the dominant NW-SE structural grain in the transition zone from Precambrian to Phanerozoic Europe. The fault is located along the extension of the boundary between the Sarmatia and Fennoscandia segments of the East European Craton (EEC). While Late Cretaceous fault activity has been documented by studies since the 1980s, its earlier history remains poorly understood. To better understand the deep crustal structure and its link to shallow deformation, new magnetotelluric data from 39 points, along with older geomagnetic data from 22 survey points, were used to create a three-dimensional (3-D) model of the geoelectric structure.

AutorzyNadine J. Kanik, Artur Kuligiewicz, Jeffrey T. Cullen
Rok2024
TytułImpacts of chemical pre-treatments on the hydrogen isotope composition of clay minerals: Determining potential effects in the absence of impurities
CzasopismoApplied Clay Science, Volume 247, 2024
DOIhttps://doi.org/10.1016/j.clay.2023.107213

Highlights

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AutorzySzczepański J, Kaszuba G, Anczkiewicz R, Ilnicki S.
Rok2023
TytułProvenance of the early Palaeozoic volcano-sedimentary successions from eastern part of the Central Sudetes: implications for the tectonic evolution of the NE Bohemian Massif.
CzasopismoGeological Magazine. 2023;160(8):1498-1534.
DOIhttps://doi.org/10.1017/S0016756823000523

The Kamieniec Metamorphic Belt (KMB) and the Doboszowice Metamorphic Complex (DMC) expose a fragment of the pre-Variscan volcano-sedimentary cover preserved in the Fore-Sudetic Block in the NE part of the Bohemian Massif. We present the age of detrital and magmatic zircon grains and the bulk rock chemical composition of rock samples from the KMB and the DMC to better understand the evolution of the early Palaeozoic Gondwana margin.

Autorzy Christopher J Barnes, Mattia Gilio, Michał Bukała, Adam Włodek, Jarosław Majka, Matthijs Smit
Rok2023
TytułGarnet–Quartz Inclusion Thermobarometry and Lu–Hf Chronology Detail the Pre-Ultra-High Pressure Metamorphic History of the Grapesvare Nappe, Scandinavian Caledonides
Czasopismo Journal of Petrology, Volume 64, Issue 12
DOIhttps://doi.org/10.1093/petrology/egad086

The subduction–exhumation history of the Grapesvare nappe in the northern Seve Nappe Complex (Scandinavian Caledonides) is recorded by late Cambrian/Early Ordovician ultra-high pressure (UHP) and subsequent amphibolite facies metamorphic events. Records of these events obscured earlier metamorphic episodes that are important for understanding the tectonics of the orogen. To extract the pre–UHP metamorphic records, garnet Lu–Hf geochronology, Titanium-in-Quartz thermobarometry, and Quartz-in-Garnet elastic thermobarometry were applied to garnet porphyroblasts in metasedimentary rocks and eclogite.

Autorzy Jan Środoń, Daniel J. Condon, Elena Golubkova, Ian L. Millar, Oksana Kuzmenkova, Mariusz Paszkowski, Stanisław Mazur, Artur Kędzior, Daniel Drygant, Valerian Ciobotaru, Sirle Liivamägi
Rok2023
TytułAges of the Ediacaran Volyn-Brest trap volcanism, glaciations, paleosols, Podillya Ediacaran soft-bodied organisms, and the Redkino-Kotlin boundary (East European Craton) constrained by zircon single grain U-Pb dating
CzasopismoPrecambrian Research, Volume 386, March 2023, 106962
DOIhttps://doi.org/10.1016/j.precamres.2023.106962

  Combined single zircon crystal CA-ID-TIMS U-Pb dating, micropaleontological study, and quantitative XRD analysis were used to correlate sections of the Podillya-Moldova Ediacaran succession with sections of the Volyn Large Igneous Province (Volyn LIP). Five U-Pb zircon ages were obtained from Volyn LIP rocks, and four from three distinct Podillya bentonite horizons. Biostratigraphic determinations were made for one section in Volyn, and two sections in Podillya. It was concluded that Volyn LIP activity had two phases.

Autorzy Helena Hercman, Michał Gąsiorowski, Jacek Szczygieł, Pavel Bella, Michał Gradziński, Marcin Błaszczyk, Šárka Matoušková, Petr Pruner, Pavel Bosák
Rok2023
TytułDelayed valley incision due to karst capture (Demänová Cave System, Western Carpathians, Slovakia) Trough in Central Poland
CzasopismoGeomorphology, Volume 437, 15 September 2023, 108809
DOIhttps://doi.org/10.1016/j.geomorph.2023.108809

Karst systems can control the amount of water flowing on the surface and thus the fluvial erosional efficiency. Here, we used the ages of speleothems from the active cave system to determine the middle Pleistocene history of the entrenchment of the Demänová Valley.

Autorzy Gąsiorowski, M., Sienkiewicz, E., Kowalewska, U.
Rok2023
TytułPaleohydrological changes during the Late Holocene recorded in the sediments of two mountain lakes in the Tatra Mountains (Central Europe)
CzasopismoJournal of Paleolimnology 70, 293–310 (2023)
DOIhttps://doi.org/10.1007/s10933-023-00294-9

Changes in local hydrological and climatic conditions over the last 5500 years have been reconstructed based on geochemical and paleobiological features recorded in the sediments of two mountain lakes.

AutorzyBudzyń, B., Wirth, R., Sláma, J., Kozub-Budzyń, G.A., Schreiber, A.
Rok2023
TytułAtomic-scale Th and U segregation into dislocation cores and U-Pb age discordance in xenotime.
CzasopismoLithos, 444–445, 107105
DOIdoi:10.1016/j.lithos.2023.107105

Highlights:
•    dislocation cores in xenotime contain U, Th and Si enriched material
•    dislocations are surrounded on both sides by radiation-damaged xenotime
•    transport of U in dislocations network is a suggested source of age discordance

AutorzyWysocka I., Kaczor-Kurzawa D., Porowski A.
Rok2022
TytułDevelopment and validation of seaFAST-ICP-QMS method for determination of rare earth elements total concentrations in natural mineral waters
CzasopismoFood Chemistry, Volume 388, 133008 (2022)
DOIhttps://doi.org/10.1016/j.foodchem.2022.133008

Highlights

• The seaFAST-ICP-QMS method is used for REE analyses in natural mineral waters.

• Method validation and characteristic parameters are presented and discussed.

• Potential of REE distribution in bottled waters for their authentication is shown.

• REE patterns in native and bottled mineral waters are compared.

• All REE concentrations in the reference samples SERMIN1 and VIDAC18 are presented.

 

 

 

AutorzyKaczor-Kurzawa D., Wysocka I., Porowski A., Drzewicz P., Vassileva E
Rok2022
TytułThe occurrence and distribution of rare earth elements in mineral and thermal waters in the Polish Lowlands
CzasopismoJournal of Geochemical Exploration, Volume 237, June 2022, 106984
DOIhttps://doi.org/10.1016/j.gexplo.2022.106984

Highlights

• REE contents and three REE-pattern types were determined in waters studied.

• Combination of seaFAST system and ICP-MS detection for REE analyses in waters

• REE-patterns in water and aquifer host rocks were used to assess REE-fractionation.

• Ce and Eu anomalies revealed different geochemical conditions in aqueous systems.