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Wyświetlanie 1-2 z 2
Tytuł:
Multivariate S-wave velocity prediction in the assessment of elastic parameters in shale formations
Autorzy:
Kaczmarczyk, Weronika
Słota-Valim, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/1833906.pdf
Data publikacji:
2020
Wydawca:
Instytut Nafty i Gazu - Państwowy Instytut Badawczy
Tematy:
fala poprzeczna
formacje łupkowe
basen bałtycki
parametry sprężyste
shear wave
shale formations
Baltic basin
elastic properties
Opis:
Exploration and development of the hydrocarbons reservoir in unconventional rock formation is a huge challenge. Due to their specific nature, which is manifested by limited filtration properties, they require an appropriate approach and the use of specific solutions. They include, among others, the determination of zones with higher hydrocarbon potential – so called sweet spots, application of horizontal drilling technology, or designing as well as performing rock stimulation treatments of rocks usually with low or almost zero permeability with the use of hydraulic fracturing. The analysis of the right combination of parameters in this case can be essential and provide extremely important information about the reservoir in an unconventional rock formation. As one of the most important parameters allowing, among others, to characterize the reservoir in terms of rock susceptibility to hydraulic fracturing, elastic properties require the availability of shear wave Vs, which in contrast to compressional wave Vp in the Polish standard is measured rarely. Therefore, in this paper, a multivariate prediction of shear wave velocity was developed with the use of theoretical models known from the literature and modified, based on which we estimate the elastic parameters. Using the obtained results, the elastic parameters were calculated on the basis of which, in the next stage, interdisciplinary characterization of reservoir formation is possible, e.g. in the aspect of assessing the reservoir formation susceptibility to hydraulic fracturing and thus creating technological fractures constituting the migration path for reservoir fluids. Based on different solutions, 5 variants of shear wave velocity were developed in the borehole scale, the results of which were then used to calculate the elastic modules: the Young modulus and the Poisson ratio. Because of the availability of the measured shear wave in each analyzed wellbores, it was possible to verify the results of the estimated variants. Subsequently, for the purpose of spatial characterization of the reservoir, calculated variants of the Young modulus were integrated with the seismic data. The analysis was conducted in Ordovician – Silurian shale formations in the Baltic Basin, at intervals enriched with organic matter.
Źródło:
Nafta-Gaz; 2020, 76, 7; 441--448
0867-8871
Pojawia się w:
Nafta-Gaz
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Marine snow and epipelagic suspensoids in the Reda carbonates and a pronounced mid-Ludfordian (Silurian) CIE in the axis of the Baltic Basin (Poland)
Autorzy:
Kozłowski, Wojciech
Powiązania:
https://bibliotekanauki.pl/articles/1835581.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
pelagic carbonates
Sparoids
marine snow
algal blooms
eolian dust
carbonate supersaturation
euxinia
Baltic basin
Reda Member
ludlow
Silurian
węglany pelagiczne
sparoidy
śnieg morski
zakwit glonów
osady eoliczne
basen bałtycki
sylur
Opis:
The mid-Ludfordian pronounced, positive carbon isotope excursion (CIE), coincident with the Lau/kozlowskii extinction event, has been widely studied so far in shallow-water, carbonate successions, whereas its deep-water record remains insufficiently known. The aim of this research is to reconstruct the sedimentary environments and the palaeoredox conditions in the axial part of the Baltic-Podolian Basin during the event. For these purposes, the Pasłęk IG-1 core section has been examined using microfacies analysis, framboid pyrite diameter and carbon isotope measurements. The prelude to the event records an increased influx of detrital dolomite interpreted as eolian dust, coupled with a pronounced decrease in the diameter of the pyrite framboids, indicating persistent euxinic conditions across the event. The event climax is recorded as the Reda Member and consists of calcisiltites, composed of calcite microcrystals (‘sparoids’), which are interpreted as suspensoids induced by phytoplankton blooms in the hipersaturation conditions present in the epipelagic layer of the basin. Both the prelude and climax facies show lamination, interpreted as having resulted from periodical settling of marine snow, combined with hydraulic sorting within a ‘benthic flocculent layer’, which additionally may be responsible for a low organic matter preservation rate due to methanogenic decomposition. Contrary to the observed basinward CIE decline in the benthic carbonates in the basin, the Reda Member records an extremely positive CIE (up to 8.25‰). Given the pelagic origin of the sparoids, the CIE seems to record surface-water carbon isotope ratios. This points to a large carbon isotope gradient and kinetic fractionation between surface and bottom waters during the mid-Ludfordian event in a strongly stratified basin. The Reda facies-isotope anomaly is regarded as undoubtedly globally triggered, but amplified by the stratified and euxinic conditions in the partly isolated, Baltic-Podolian basin. Hence, the common interpretation of the basin record as representative for the global ocean needs to be treated with great caution.
Źródło:
Acta Geologica Polonica; 2020, 70, 4; 529-567
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
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