Assessment of thermal evolution of Paleozoic successions of the Holy Cross Mountains (Poland)

Schito, Andrea; Corrado, Sveva; Trolese, Matteo; Aldega, Luca; Caricchi, Chiara; Cirilli, Simonetta; Grigo, D.; Guedes, Alexandra; Romano, Cláudia; Spina, Amalia; Valentim, Bruno

doi:10.1016/j.marpetgeo.2016.11.016

Cited by 48 publications

(21 citation statements)

References 62 publications

(130 reference statements)

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“…Either detrital and neoformed minerals in the <2 µm grain-size fraction were investigated in order to determine the maximum burial conditions the fault rocks underwent during thrusting. In particular, mixed layers illite-smectite (I-S) can be used as indicators of the thermal evolution of sedimentary successions (Aldega et al, 2007;2014;Corrado et al, 2010;Izquierdo-Llavall et al, 2013), for evaluating the amount of denudation of the sedimentary and/or tectonic overburden, removed by erosion and/or tectonics (Aldega et al, 2011;Di Paolo et al, 2012, Caricchi et al, 2015Schito et al, 2017) and determining the depth at which deformation occurred in fold-and-thrust belts (Meneghini et al, 2012, Carlini et al, 2013, Carminati et al, 2013.…”

Section: X-ray Diffraction Of Fault Rocksmentioning

confidence: 99%

Strain indicators and magnetic fabric in intraplate fault zones: Case study of Daroca thrust, Iberian Chain, Spain

et al. 2018

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Anisotropy of magnetic susceptibility (AMS) has been applied to the study of shallow fault zones, although interpretation of the results requires establishing clear relationships between petrofabric and magnetic features, magnetic behavior of fault rocks, and an extensive knowledge of P-T conditions. In this work, we demonstrate that magnetic methods can be applied to the study of heterogeneous fault zones, provided that a series of requisites are met. A major fault zone within the Iberian plate (Daroca thrust), showing transpressional movements during Cenozoic time was chosen for this purpose, because of the exceptional outcrops of fault gouge and microbreccia and its relevance within the context of the northeastern Iberian Plate. Magnetic fabrics were analysed and the results were compared with foliation and S-C structures measured within the fault zone. Clay mineral assemblages suggest maximum burial depths shallower than 2 km (<60-70°C) for fault rocks in the footwall of the Daroca thrust. The orientation of the AMS axes is consistent with mesostructural strain indicators: k min parallels the mean pole to S, or it is intermediate between S and C poles; k max is oriented at a high angle (nearly orthogonal in overall) to the transport direction, which can be explained from both deformational and mineralogical controls. Both magnetic fabrics and kinematic indicators are consistent with a reverse movement for most of the fault zone.

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Section: X-ray Diffraction Of Fault Rocksmentioning

confidence: 99%

Strain indicators and magnetic fabric in intraplate fault zones: Case study of Daroca thrust, Iberian Chain, Spain

et al. 2018

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“…Schito et al. () 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., ).…”

Section: Introductionmentioning

confidence: 99%

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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“…Ferralis et al [136] reported a linear relationship between the Raman spectral parameters of fossil organic matter and the H:C value (0.01-0.65). Bonoldi et al [134] and Schito et al [137] demonstrated that Raman spectroscopy can be used to assess the thermal maturity of organic matter devoid in vitrinite such as lower Paleozoic source rocks. Henry et al [138] studied the effects of sample preparation and measurements on Raman spectra for the assessment of the maturity of organic matter in shale, and the results showed that for low maturity (R r < 0.6%) samples, it is recommended to using third-order polynomial for baseline calibration, whereas deconvolution analysis for spectral curves is not recommended.…”

Section: Study Of Coal Rankmentioning

confidence: 99%

Progress of Raman spectroscopic investigations on the structure and properties of coal

Xia

Wang

et al. 2020

J Raman Spectroscopy

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Raman spectroscopy is a nondestructive and in situ analytical technique that could provide information on the chemical structure and structural ordering of carbonaceous materials. Based on the E2g symmetric stretching vibration mode in the aromatic layers (G band, ~1,580 cm−1) and the defect structure in graphite (D band, ~1,350 cm−1), Raman spectroscopy has been used extensively to characterize the structural features of carbonaceous matters since 1970. Coal is a complex organic compound made up mainly by carbon showing characteristic Raman bands. This article reviews the application of Raman spectroscopy for coal structure characterization under room temperature, to determine its chemical structure, crystallite size, coal rank, and combustion reactivity. Future research for collecting Raman spectra during coal pyrolysis at high temperatures is also discussed. The combination of high‐temperature hot stage with Raman spectroscopy technology allows direct collection of Raman spectra at high temperature.

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Assessment of thermal evolution of Paleozoic successions of the Holy Cross Mountains (Poland)

Cited by 48 publications

References 62 publications

Strain indicators and magnetic fabric in intraplate fault zones: Case study of Daroca thrust, Iberian Chain, Spain

Strain indicators and magnetic fabric in intraplate fault zones: Case study of Daroca thrust, Iberian Chain, Spain

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

Progress of Raman spectroscopic investigations on the structure and properties of coal

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