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O analizach kratownicy ze ściskanym pasem dolnym

Krajewski Marcin

Inżynieria i Budownictwo

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2020

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R. 76, nr 1-2

92--95

PL

Przedstawiono rezultaty analiz nośności kratownicy poddanej obciążeniu od wiatru. Wykonano liniowe analizy stateczności modelu prętowego i powłokowego konstrukcji przy różnych warunkach brzegowych na podporach skrajnych. Badano wpływ sztywności (rotacyjnej) stężeń pasa górnego na nośność konstrukcji. Zaprezentowano model pasa dolnego, podpartego sprężyście, jako model zastępczy kratownicy przestrzennej. Przedstawiono rezultaty analiz statycznych, nieliniowych, przeprowadzonych dla konstrukcji z imperfekcjami.

EN

In the paper the load bearing capacity analysis of the truss subjected to upward wind loading were presented. The linear buckling analysis results for the beam and shell model of the structure, due to various boundary condition at the marginal supports, were appointed. The influence of the top chord brace stiffness (rotational) on the capacity of the truss, was taken into consideration. The model of the bottom chord on elastic supports was presented as the replacement for the spatial structure. The nonlinear static analysis for the imperfect truss model was carried out.

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Lower Kimmeridgian facies and sedimentary succession of a shallow-water coated-grain-dominated carbonate ramp of the northern peri-Tethyan shelf : an example from the Radomsko Folds (central Poland)

Olchowy Piotr, Krajewski Marcin

Geological Quarterly

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2020

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Vol. 64, No. 4

969--987

EN

An Upper Jurassic succession is exposed in the active Rogaszyn Quarry (Kodrąb area) located in the Radomsko Folds structure (central Poland). Six facies types were distinguished, comprising oolitic, oncolitic, biodetrital and pelitic limestones as well as marls and marly clays. Typical lithologies are limestones with coated grains deposited in shallow-water, fore-shoal, shoal and lagoonal parts of a carbonate ramp. Three types of ooid and three types of oncoid were identified, which display several shapes and sizes, and a complex structure of cortices. The ooid types show micritic, radial-fibrous and mixed, micritic/radial-fibrous cortices. Type 1 oncoids comprise micritic or bioclastic nuclei enveloped by non-laminated or laminated micritic cortices. Type 2 oncoids are composed of micritic or bioclastic nuclei and laminated, fossil-bearing cortices covered by microbial envelopes. Type 3 oncoids are the largest of the oncoids observed, attaining cm-scale dimensions. These oncoids are formed of a Bacinella-dominated meshwork incorporating smaller ooids and oncoids, or they have bioclastic or micritic nuclei covered by complex cortices with micritic, laminated, fossil-bearing, Bacinella-dominated fabric and microbial envelopes. Boundaries between the specific types of cortical envelopes are usually sharp and accentuated by organic encrustations, elongated bioclasts or borings. Commonly found are chambers of the ichnogenus Entobia representing the boring traces of carbonate-excavating sponges and the cryptoendolithic foraminifer Troglotella incrustants. The complex cortices indicate different growth stages of oncoids at different conditions of currents and microbial activity. Carbonate deposition was accompanied by mixed siliciclastic-carbonate sedimentation resulting in multiple intercalated layers of marls and pelitic limestones as well as marly clays. The deposits exposed in the Rogaszyn Quarry as well as in the Kodrąb area are compared with the neighbouring Upper Jurassic deposits of the Szczerców area and the Sw margin of the Holy Cross Mts. (both central Poland). The successions from the Kodrąb area are generally similar to the Lower Kimmeridgian sequences known from adjacent areas, but with locally observed facies variability.

3

Late Jurassic facies succession of the Kleszczów Graben area (southern border of the Łódź Depression, peri-Tethyan shelf, central Poland)

Olchowy Piotr, Krajewski Marcin, Felisiak Ireneusz

Geological Quarterly

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2019

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Vol. 63, No. 4

657--682

EN

Numerous fully cored boreholes completed in the last years in central Poland (Kleszczów Graben area, southern border of the Łódź Depression) enabled the researchers to obtain new sedimentological data on the Oxfordian-Tithonian continuous sedimentary record in the Polish part of the northern Tethys shelf. Twenty-two facies were distinguished in the sedimentological succession. The facies represent the outer-, mid- and inner-ramp environments, including evaporitic episodes and palaeosols. The facies document that the Oxfordian-Lower Kimmeridgian (up to Hypselocyclum) carbonate ramp has evolved to the Upper Kimmeridgian-Tithonian carbonate-siliciclastic ramp. Among the Kimmeridgian deposits, numerous hardgrounds, tidal channel deposits and gravity flow sediments were identified. The Kleszczów Graben sedimentary succession is discussed along with the lithostratigraphical units known from the adjacent regions of southern and central Poland.