Wyniki wyszukiwania - Biblioteka Nauki

Nowa wersja platformy, zawierająca wyłącznie zasoby pełnotekstowe, jest już dostępna.
Przejdź na https://bibliotekanauki.pl

Ograniczanie wyników

Znaleziono wyników: 3

Liczba wyników na stronie

Wyniki wyszukiwania

Sortuj według:

Ogranicz wyniki do:

Depositional environment and petrology of Rotliegend deposits from the Unisław-Wałdowo Królewskie region

100%

Buniak A. , Mikołajewski Z. , Protas A.

Geologos

1999

tom Vol. 4

5--27

The Rotliegend deposits have been drilled in following boreholes: Unisław 2, Unisław 4, Unisław IG1, Unisław IG2 and Wałdowo Królewskie 1. In studied area these sediments constitue a differentiated lithological complex, being a product of varied depositional conditions, controlled mainly by tectonics and paleoclimatic factors. Two general facies associations: lacustrine and fluvial ones have been distinguished. Lacustrine facies is dominated by claystones, siltstones and fine sandstones originated in seasonally dried lake basin but fluvial sediments are represented by varigrained sandstones accumulated as channel and sheet flood deposits. Two phases of Rotliegend deposition were defined: the first one of a fluvial character and the second one with expansion of lacustrine facies. Evolution of porosity was controlled by cementation processes and low reservoir properties of lacustrine deposits are a consequence of their development and rich matrix content. Fluvial sediments are considered as a potential reservoir rock, with higher reservoir characteristics.

Utwory czerwonego spągowca przewiercono w otworach wiertniczych Unisław 2, Unisław 4, Unisław IG1, Unisław IG2 oraz Wałdowo Królewskie 1. Na omawianym obszarze stanowią one zróżnicowany kompleks litofacjalny będący efektem zmiennych warunków depozycji, na które decydujący wpływ miały tektonika i warunki paleoklimatyczne. Opisano następujące zespoły facjalne: zespół osadów jeziornych i zespół osadów fluwialnych. Wśród osadów jeziornych dominują iłowce, mułowce i piaskowce drobnoziarniste powstałe w okresowo wysychającym zbiorniku jeziornym, natomiast osady fluwialne reprezentowane są przez różnoziarniste piaskowce powstałe w facjach korytowych oraz jako pozakorytowe zalewy warstwowe. Depozycja utworów czerwonego spągowca przebiegała w dwóch etapach. W pierwszym dominowała działalność fluwialna, w drugim etapie obserwujemy przekraczające występowanie osadów zbiornika jeziornego. Stwierdzono dominujący wpływ procesów cementacji w modelowaniu przestrzeni porowej. Niskie własności zbiornikowe osadów jeziornych związane są z ich wykształceniem oraz obecnością obfitego matriks. Osady fluwialne są potencjalną skałą zbiornikową, posiadają wyższe własności zbiornikowe.

Thermal history of Lower Palaeozoic rocks from the East European Platform margin of Poland based on K-Ar age dating and illite-smectite palaeothermometry - 481 – 509

75%

Kowalska S. , Wójtowicz A. , Hałas S. , Wemmer K. , Mikołajewski Z. , Buniak A.

Annales Societatis Geologorum Poloniae

2019

tom Vol. 89, No. 4

481--509

Large-scale shale gas prospecting in the Polish part of the East European Platform did not discover large reserves of this resources. The article presents new research indicating that one of the reasons for the lack of shale gas relates to the thermal history of the Lower Palaeozoic rocks. Illite-smectite palaeothermometry was used to reconstruct the history of the platform and determine the maximum temperatures to which these rocks were subjected. The age of illitisation was also constrained using the K-Ar method. This method allowed precise dating of the maximum age of thermal transformations due to the deposition of numerous pyroclastic horizons (K-bentonite) throughout the entire geological profile from the Cambrian to the Silurian. Isotopic dating was made on over 53 samples of Lower Palaeozoic bentonites and low-grade metamorphic clays. These results were supplemented by analysis of the degree of thermal (smectite to illite) transformation in the profiles of 37 deep boreholes. 11 zones could be distinguished with different tectonic histories within the Polish part of the East European Platform edge. Maximum heating occurred in this region at about 320–340 Ma, corresponding to the Early Carboniferous or the turn of the Early and Late Carboniferous, phase A of the Variscan orogeny, known as the Sudetian phase. In the southern part of study area, the maximum of thermodiagenesis is slightly younger – 270–290 Ma, which responds to the Early Permian, the Asturian phase, the last phase of the Variscan orogeny. This means that the generation of hydrocarbons occurred before significant Mesozoic exhumation of the Polish part of the East European Platform, which led to the escape of a considerable amount of the gas generated. The study also presents the results of an interlaboratory comparison of illite age dating using the K-Ar and Ar-Ar methods. The comparison was conducted to find out what realistic error should be considered when interpreting geological K-Ar dating results.

An evaluation of the impact of shot and receiver lines spacing on seismic data quality – the Wierzbica 3D AGH seismic experiment

75%

Barmuta J. , Korbecka M. , Hadro P. , Pieniądz K. , Stefaniuk M. , Dzwinel K. , Buniak A.

Geology, Geophysics and Environment

2020

tom Vol. 46, no. 2

93--108

An attempt was made to describe the quality of the stacked seismic data semi-quantitatively with respect to the spacing of shot and receiver lines. The methods used included: signal-to-noise ratio calculation, seismic-to-well tie accuracy, wavelet extraction effectiveness and reliability of semi-automated interpretation of seismic attributes. This study was focused on the Ordovician-Silurian interval of the Lublin Basin, Poland, as it was considered as a main target for the exploration of unconventional hydrocarbon deposits. Our results reconfirm the obvious dependency between the density of the acquisition parameters and data quality. However, we also discovered that the seismic data quality is less affected by the shot line spacing than by comparable receiver line spacing. We attributed this issue to the fact of the higher irregularity of the shot points than receiver points, imposed by the terrain accessibility. We have also proven that the regularity of receiver and shot point distribution is crucial for the reliable interpretation of structural seismic attributes, since these were found to be highly sensitive to the acquisition geometry.