Raman spectroscopic and microthermometric studies of authigenic quartz (the Pepper Mts., Central Poland) as an indicator of fluids circulation

Naglik, Beata; Toboła, Tomasz; Natkaniec‐Nowak, Lucyna; Luptáková, Jarmila; Milovská, Stanislava

doi:10.1016/j.saa.2016.10.047

Cited by 3 publications

(4 citation statements)

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“…Advective heat transfer by fluid migration along the HCF zone has already been postulated by Naglik et al. (), Narkiewicz et al. () and Poprawa et al.…”

Section: Discussionmentioning

confidence: 61%

“…The HCF had a clear imprint on the maturity pattern created during the Variscan shortening of the HCM (Naglik et al., ; Narkiewicz et al., ; Poprawa et al., ) presumably providing a conduit for hydrothermal solutions circulating at that time. However, during the Late Cretaceous–earliest Palaeogene inversion, vertical displacements along the fault were probably too small to influence the maturity distribution as suggested from the thermal modelling results of samples from both sides of the fault (Figure b,c).…”

Section: Discussionmentioning

confidence: 99%

“…There is no consensus on the tectonothermal evolution of the HCM and several contradicting models have been proposed. Most authors (Bełka, ; Marynowski, , ; Marynowski, Salamon, & Narkiewicz, ; Naglik, Toboła, Natkaniec‐Nowak, Luptáková, & Milovská, ; Narkiewicz, ; Narkiewicz, Resak, Littke, & Marynowski, ; Smolarek, Marynowski, Spunda, & Trela, ) argue for an elevated Variscan (late Carboniferous to early Permian) heat flow, which significantly exceeded the current low values (Szewczyk & Gientka, ). However, Poprawa, Żywiecki, and Grotek () proposed that thermal maturity of organic matter in the Devonian to Jurassic sedimentary successions was achieved during Late Jurassic or Late Cretaceous burial that was characterized by constant heat flow equal to the recent one (Szewczyk & Gientka, ).…”

Section: Introductionmentioning

confidence: 99%

“…() presented burial and thermal history models, assuming very low constant heat flow during the Palaeozoic to Jurassic that subsequently increased up to the present‐day values from the Early Cretaceous onwards with maximum palaeotemperatures reached in the Late Cretaceous. Most authors agree about a key role of the HCF in controlling the Variscan thermal regime within the region (Bełka, ; Marynowski, ; Poprawa et al., ) and enhancing Carboniferous–Permian advective heat flow by fluid migration (Naglik et al., ; Narkiewicz et al., ; Poprawa et al., ). In the HCM, burial and exhumation events of different magnitudes can be related to the HCF polyphase activity.…”

Section: Introductionmentioning

confidence: 99%

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Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low‐temperature thermochronology

et al. 2018

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The low-temperature thermal history of the Holy Cross Mountains (HCM) is investigated by apatite fission track and apatite and zircon (U-Th)/He thermochronology.Our results provide constraints on the deformation history of Palaeozoic basement rocks in the transition area from Precambrian to Palaeozoic Europe that are exposed from beneath Permian-Mesozoic sediments within the HCM. Late to post-Variscan cooling of the Palaeozoic strata from maximum temperatures is shown to be a major feature of the HCM. This cooling likely followed a heating event related to burial and/or hot fluid circulation along the Holy Cross Fault in the late Carboniferous.The central part of the HCM shows a rapid cooling event caused by tectonic inversion, which started in the Late Cretaceous. However, this event was less pronounced in the western margin of the HCM, where slow cooling continued throughout the Mesozoic with only minor acceleration of the cooling rate since the latest Cretaceous.

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“…Advective heat transfer by fluid migration along the HCF zone has already been postulated by Naglik et al. (), Narkiewicz et al. () and Poprawa et al.…”

Section: Discussionmentioning

confidence: 61%

Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low‐temperature thermochronology

et al. 2018

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In situ high temperature spectroscopic study of liquid inclusions and hydroxyl groups in high purity natural quartz

Gaweł

Ulvensøen

Łukaszuk

et al. 2021

Minerals Engineering

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The Holy Cross Mountains (Poland) terranes palaeoposition and depositional environment in Silurian—new insights from rock magnetic studies

Niezabitowska

Szaniawski²

2023

Geophysical Journal International

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Summary The Holy Cross Mountains (HCM) in Poland, is an isolated natural outcrop of Paleozoic rocks located within the Trans-European Suture Zone (TESZ), a tectonic collage of continental terranes adjacent to the Tornquist margin of the Baltica. This uniqueness made the HCM a target for paleogeographic research. Based on the facies differences, the HCM had been divided into two major units, the southern (the Kielce Unit) and northern (the Łysogóry Unit) part (SHCM and NHCM, respectively). Their position in relation to each other and the Baltica continent during Silurian times is still a matter of discussion, whether both parts of the HCM were separated terranes located along the Baltica margin or they shared in common paleogeographic history. Here, we present the results of comprehensive rock magnetic measurements applied as a tool to interpret paleoenvironmental conditions during deposition and burial and therefore allow discussion about the terranes’ relative position. To recognize the magnetic mineral composition and texture of studied Silurian graptolitic shales several rock magnetic measurements were conducted including low-temperature Saturated Isothermal Remanent Magnetization (SIRM), thermal demagnetization of three-component IRM, and hysteresis measurements, as well as anisotropy of magnetic susceptibility (AMS). The sampled rocks come from both units of the HCM. In all analyzed samples we found single domain (SD) stoichiometric magnetite of mostly diagenetic (i.e., postdepositional) origin and goethite resulting likely from weathering. In turn, detrital magnetite, even if observed in previously investigated Silurian rocks from the Baltica margin, was not identified in this study, what we attribute to dissolution during diagenesis in the deep-water environment. Solely in the NHCM, SD hematite and maghemite grains were observed, which we interpret as detrital in origin. These grains have been preserved in the suboxic environment of the NHCM sub-basin bottom waters due to their resistance to dissolution in marine waters. Considering the deposition conditions (oxygenation of the near-bottom zone) rather similar for both HCM parts, we associate the presence of aeolian hematite grains solely in the NHCM rocks with a more proximal position of the NHCM than the SHCM in relation to the Baltica continent during late Llandovery (Silurian). This conclusion agrees with some existing paleogeographic models. In addition to petromagnetic studies focused on the analysis of ferromagnets, AMS measurements were also carried out. The results indicate that the magnetic susceptibility is mainly governed by paramagnetic minerals, mostly phyllosilicates with small ferromagnetic contributions. Oblate AMS ellipsoid and distinct bedding parallel foliation indicate prevailing sedimentary-compactional alignment. Observed magnetic lineation of tectonic origin resulting from weak strain is related presumably to Variscian deformations.

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Raman spectroscopic and microthermometric studies of authigenic quartz (the Pepper Mts., Central Poland) as an indicator of fluids circulation

Cited by 3 publications

References 10 publications

Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low‐temperature thermochronology

Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low‐temperature thermochronology

In situ high temperature spectroscopic study of liquid inclusions and hydroxyl groups in high purity natural quartz

The Holy Cross Mountains (Poland) terranes palaeoposition and depositional environment in Silurian—new insights from rock magnetic studies

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