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Wyszukujesz frazę "breakouts" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Present-day stress profile in the Baltic Basin sedimentary succession constrained by drilling-induced structures : interpretation uncertainties
Autorzy:
Piłacik, Alicja
Jarosiński, Marek
Powiązania:
https://bibliotekanauki.pl/articles/2058697.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
recent stress profile
borehole wall stability
breakouts
shale geomechanics
Opis:
A far-field stress model based on theory of elasticity and utilizing the Mohr-Coulomb criterion is commonly used in the petroleum industry as a reliable method for present-day stress profiling. We have analysed the present-day stress profile in the Lower Paleozoic shale succession of the Baltic Basin (northern Poland), Based on data from a single borehole. Our analyses take into account the vertical transverse isotropy (VTI) of the mechanical properties. Initial modelling of the stress profile showed - despite general agreement concerning the length and location of the modelled and observed breakouts - systematic differences when the profile of these structures is analysed in detail. Analyses carried out for selected segments of the borehole have shown that the mere presence of breakouts affects the interpretation of the mechanical properties, and thus also the stress profile. We have analysed the size of the necessary correction for tectonic strain, to avoid this effect, as well as uncertainty resulting from the failure criteria adopted. The final model, corrected for stress disturbances by breakouts, reveals the strati fication of stress regime, with the dominance of a normal faulting regime, and low values of differential stresses in the shale formations.
Źródło:
Geological Quarterly; 2021, 65, 4; 71--88
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Recent tectonic stress field investigations in Poland : a state of the art
Autorzy:
Jarosiński, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059238.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polska
recent geodynamics
tectonic stress
borehole breakouts
hydraulic fracturing
modelling
Opis:
The paper summarizes up-to-date knowledge of the contemporary tectonic stress field in Poland and compares the results of geophysical measurements with mathematical models. The extensive set of data provided by borehole breakout analyses is supplemented by hydraulic fracturing tests, earthquake focal mechanism solutions and preliminary resolution of regional intraplate motions from GPS measurements. Frequent breakout presence shows that tectonically driven anisotropy of horizontal stress is a common feature in the study area. Roughly N-S direction of maximum horizontal stress (SHmaxx) in Eastern Poland differs significantly from Western European stress domain. This difference is produced by tectonic push of Alcapa, which is successively compensated within the Teisseyre-Tornquist Zone (TTZ) and in the Upper Silesian segment of the Outer Carpathians. In the western part of Poland stress directions are ambiguous due to interplay of several additional tectonic factors. Most of hydraulic fracturing data and earthquake focal mechanism solutions indicate strike-slip stress regime in Eastern Poland where stresses are in equilibrium with preferentially oriented faults of Iow friction (0.16). Limited data from Western Poland suggest normal fault stress regime. Good conformity between directions of 5Hm", and intraplate motions occurs from comparison of breakout and GPS data. Finite element modelling shows that the most important factor shaping the stress field in Eastern and Central Poland is the Adria push transmitted through the Pannonian region. Secondary, but still notable factors are differentiation of loads along the Mediterranean collision zone and changes in magnitude of the ridge push force along the NW Continental passive margin of Europe. Results of rheological modelling indicate that the crust is entirely decoupled from the mantle in the Fore-Sudetic Platform, partial uncoupling in the base or the upper crust is possible in the TTZ while in the East European Craton (EEC) the whole lithosphere is coupled. The comparison of different set of data and models presented here provides a comprehensive geodynamic scenario for Poland, however, a number of unresolved questions still remains to be addressed.
Źródło:
Geological Quarterly; 2006, 50, 3; 303-321
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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