Ichnology of Upper Cretaceous deep-sea thick-bedded flysch sandstones: Lower Istebna Beds, Silesian Unit (Outer Carpathians, southern Poland)

Rajchel, Jacek; Uchman, Alfred

doi:10.2478/v10096-012-0009-3

Cited by 11 publications

(4 citation statements)

References 14 publications

(18 reference statements)

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“…The Istebna sandstones of the Lower Campanian-Maastrichtian belong to the Silesian nappe [30,31], as shown in Figure 1. They are a product of deep-sea silicoclastic sedimentation in the diverse and rapidly changing deposition environments of the channels and their outlet zones of the central cone and within the non-canalized silicoclastic apron [32][33][34].…”

Section: Geological Backgroundmentioning

confidence: 99%

Pyritization in Stone-Building Materials Modeling of Geochemical Interaction

Pękała

Musiał²,

Galek³

2022

Sustainability

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Stone-building materials, despite their natural origin, must be tested for the concentration of trace elements necessary to assess their impact on the environment and humans. In addition to basic research determining their mineral composition and structural and textural features, it is important to analyze the geochemical interactions between the material matrix and the concentration of elements that have a negative impact on the surrounding natural environment and our health. In the presented study, mineralogical and geochemical studies were carried out on the Carpathian sandstones. It was shown that the studied sandstones are represented by lithic wackes and sublithic arenites. Rocks subject to the secondary process of sulfide mineralization were observed among sublithic arenites. Pyrite in the studied geomaterials took various forms. A detailed geochemical analysis was carried out in the material in which iron sulfides acted as a binder. The research was aimed at identifying possible variations in the concentration of elements, with a particular emphasis on the contact between the silica and mineralized phases. The assessment of the geochemical interaction of iron sulfides with silica at a successively enlarged measurement was carried out using the Mamdani–Assilian fuzzy inference model.

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Section: Geological Backgroundmentioning

confidence: 99%

Pyritization in Stone-Building Materials Modeling of Geochemical Interaction

Pękała

Musiał²,

Galek³

2022

Sustainability

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“…Phycosiphon is interpreted a trace of a deposit-feeding, wormlike organism (Wetzel & Bromley, 1994). Phycosiphon occurs in continental-shelf slopes, submarine fans, turbidites, and flysch deposits (e.g., Uchman, 1998;Naruse & Nifuku, 2008;Rajchel & Uchman, 2012). Recent studies have found that Phycosiphon tracemakers are early colonizers of the upper portions of turbidite deposits when bottom waters are fully oxygenated (e.g., Wetzel & Uchman, 2001;Naruse & Nifuku, 2008).…”

Section: Ichnogenus Phycosiphon Fischer-ooster 1858mentioning

confidence: 99%

Ichnotaxonomy of the Cambrian Spence Shale Member of the Langston formation, Wellsville Mountains, Northern Utah, USA

Hammersburg

Hasiotis

Robison

2018

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“…1 and 2). The lithological-sedimentological fea tures, ichnofacies char ac ter is tics and strati graphic po si tion of the de pos its have been stud ied by a num ber of authors (e.g., Hohenegger, 1861;Liebus and Uhlig, 1902;Burtanówna, 1936;Burtanówna et al, 1937;Książ kiewicz, 1962;Unrug, 1963Unrug, , 1968Eliáš, 1970;Peszat, 1976;Menčík et al, 1983;Menčík and Tyráček, 1985;Ślączka, 1986;Żytko et al, 1989;Poprawa et al, 2002Poprawa et al, , 2004Strzeboński, 2005;Grzebyk and Leszczyński, 2006;Picha et al, 2006;Ślączka et al, 2006, 2012Golonka and Waśkowska-Oliwa, 2007;Cieszkowski et al, 2009Fe lix et al, 2009;Uchman, 2009;Rajchel and Uchman, 2012).…”

Section: Introductionmentioning

confidence: 99%

Late Cretaceous - Early Palaeogene sandy-to-gravelly debris flows and their sediments in the Silesian Basin of the Alpine Tethys (Western Outer Carpathians, Istebna Formation)

Strzeboński

2014

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The study fo cuses on Up per Cre ta ceous-Paleocene de pos its from the Beskid Śląski moun tain range in south ern Po land con sti tut ing the Istebna Beds. The Istebna Beds, also re ferred to as the Istebna For ma tion, are part of the Silesian tec tonic unit, which forms the Outer Carpathian fold-and-thrust belt (part of the Al pine-Carpathian sys tem). The re sults of qual i ta tive and quan ti ta tive lithological-sedimentological stud ies were the ba sis for the in ter pre ta tion of lithofacies types, sed i men tary pro cesses and palaeoenvironment as well as for the re con struc tion of the ar chi tec ture of the depositional sys tem. The anal ysis con ducted on the ba sis of field de scrip tion of the de pos its shows the prev a lence (nearly 70%) of siliciclastic strata rep resent ing a sand stone-con glom er ate as so ci a tion (S-C), which is the main sub ject of this work. The S-C lithofacies: sand stones, grav elly sand stones, sandy con glom er ates and con glom er ates con sti tute the de pos its formed mostly by mass grav ity-flows such as sandy-to-grav elly de bris flows. The dis tri bu tion of the coarse-clastic ma te rial in di cates a sed i ment supply from south erly di rec tions and im plies the pres ence of an ac tive source area in the rear part of the Silesian Ba sin. A succes sion of the sand stone-to-con glom er ate de pos its with the sec ond ary par tic i pa tion of other lithofacies, with a thick ness of ap prox i mately two thou sand metres, in di cates tem po rary in creased di a strophic ac tiv ity in the Silesian Ridge (source area) and the in tense de nu da tion of this area. The up lift of the alimentation area and its de struc tion co in cid ing with en forced rel ative re gres sion and the un cov er ing of the prox i mal depositional zone of the ba sin led to resedimentation of the older intrabasinal ma te rial and re peated mass de po si tion to gether with de liv ery of extraclasts of pre-ex ist ing rocks and min er als. The lithofacies de vel op ment of the sand stone-to-con glom er ate debrites and the re lated sed i men tary palaeotransport di rections sug gest an ac cu mu la tion do main in the form of a lin ear apron depositional sys tem de vel oped in a deep-wa ter set ting. Ex per i men tal mod el ling of sub aque ous sandy flows has con trib uted to a better un der stand ing of the com plex gen e sis of deep-wa ter sed i ment grav ity flows de vel op ing in depositional sys tems rich in sand ma te rial.

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Ichnology of Upper Cretaceous deep-sea thick-bedded flysch sandstones: Lower Istebna Beds, Silesian Unit (Outer Carpathians, southern Poland)

Cited by 11 publications

References 14 publications

Pyritization in Stone-Building Materials Modeling of Geochemical Interaction

Pyritization in Stone-Building Materials Modeling of Geochemical Interaction

Ichnotaxonomy of the Cambrian Spence Shale Member of the Langston formation, Wellsville Mountains, Northern Utah, USA

Late Cretaceous - Early Palaeogene sandy-to-gravelly debris flows and their sediments in the Silesian Basin of the Alpine Tethys (Western Outer Carpathians, Istebna Formation)

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