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Tytuł:
Optimal site and antenna location for UMTS - output results of 3G network simulation software
Autorzy:
Nawrocki, M.J.
Więckowski, T.W.
Powiązania:
https://bibliotekanauki.pl/articles/309253.pdf
Data publikacji:
2003
Wydawca:
Instytut Łączności - Państwowy Instytut Badawczy
Tematy:
anteny
UMTS
3G
CDMA
antenna tilt
site location
Opis:
The paper presents output results of 3G network simulation software in the area of optimal site location as well as finding optimal values of antenna tilt. The loss of capacity is shown for a wide range of tilts and different antenna directions. Nonuniform distribution of base stations has been also included in the simulation scenarios influencing system performance. All of the described parameters are especially significant to CDMA systems network planning.
Źródło:
Journal of Telecommunications and Information Technology; 2003, 1; 55-58
1509-4553
1899-8852
Pojawia się w:
Journal of Telecommunications and Information Technology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochronology of selected andesitic lavas from the King George Bay area (SE King George Island)
Autorzy:
Pańczyk, M.
Nawrocki, J.
Powiązania:
https://bibliotekanauki.pl/articles/2058742.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
West Antarctica
Eocene
40Ar-39Ar dating
magnetostratigraphy
volcanic rocks
Opis:
Volcanic rocks from the Lions Rump area, which are the basement for a sequence of glaciomarine sediments of the Polonez Cove Formation, and lava flows from the Turret Point–Three Sisters Point area were sampled for thermogeochronological and palaeomagnetic investigations. Generally, andesitic lavas from King George Bay area consist mainly of clinopyroxene (Ti-augite) orthopyroxene (hyperstene) and plagioclase phenocrysts. The groundmass comprises mostly plagioclase laths, clinopyroxene, titanomagnetite and rare orthopyroxene crystals. However, the modal content, size, shape and distribution of phenocrysts are variable and specific for each sample. The Ar-Ar plateaus ages calculated for lavas from the Lions Rump area are very homogenous and point to middle Eocene age (Lutetian, ~44.5 Ma). The similar and consistent ages for volcanic basement for that area excluded the thesis about separate tectonic evolution of the Warszawa and Kraków blocks at least since the middle Eocene. The lavas from Turret Point and Three Sister Point are younger and were emplaced during the late Eocene (Bartonian/Priabonian: 37.3 š0.4 Ma and Priabonian: 35.35 š0.15 Ma, respectively). The results of isotopic investigations are consistent with magnetic polarities of the rocks indicating that the samples from the Lions Rump area are coeval with the lower part of the C20 polarity chron whereas the sample from Turret Point can be correlated with the upper part of the C17 polarity chron
Źródło:
Geological Quarterly; 2011, 55, 4; 323-334
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pliocene age of the oldest basaltic rocks of Penguin Island (South Shetland Islands, northern Antarctic Peninsula)
Autorzy:
Pańczyk, M.
Nawrocki, J.
Powiązania:
https://bibliotekanauki.pl/articles/2058747.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Antarctica
Penguin Island
Pliocene
40Ar-39Ar dating
magnetostratigraphy
basaltic rocks
Opis:
The Penguin Island volcano is located on the southern shelf of King George Island (South Shetland Islands, West Antarctica). Its activity is regarded as connected with the opening of the Bransfield Strait. Penguin Island is dominated by a 180 m high basaltic stratocone (Deacon Peak) with a 350 m wide crater containing a small basaltic plug inside and radial dykes, and it has a second principal vent – the Petrel Crater maar – that was formed during a phreatomagmatic eruption about 100 years ago. A low-potassium, calc-alkaline sequence of basaltic lava flows with intercalations of beach deposits (Marr Point Formation) forms the basement of the stratocone. The Marr Point Formation lava flows have never been dated before. Combined whole rock 40Ar-39Ar isotopic dating and magnetostratigraphy were applied for this purpose. We obtained an isotopic 40Ar-39Ar plateau age of 2.7 š0.2 Ma, and together with the palaeomagnetic data, middle Pliocene age (Piacenzian) is implied for the basaltic plateau of Penguin Island.
Źródło:
Geological Quarterly; 2011, 55, 4; 335-344
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Tournaisian 40Ar/39Ar age for alkaline basalts from the Lublin Basin (SE Poland)
Autorzy:
Pańczyk, M.
Nawrocki, J.
Powiązania:
https://bibliotekanauki.pl/articles/2059639.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
alkaline basaltic rocks
Ar-Ar geochronology
Carboniferous
Lublin Basin
Opis:
The main aim of this study is to define precisely the age of the alkaline basalts occurring within the lowermost part of Carboniferous succession in the northeastern part of LublinBasin(drill core Parczew IG-7 and IG-9; SE Poland). The new, whole-rocks 40Ar/39Ar data constrain the age of volcanic activity and emplacement of alkaline basalts to the Late Tournaisian (348 ± 0.8 Ma) with possible prolongation to the Middle Visean (338.5 ± 0.7 Ma). The younger age is however of evidently poorer quality than the older one. The new data caused to correlate the volcanic processes occurring within the Lublin Basin with alkaline intrusions drilled inNE Poland inside the Paleozoic cover of the East European Platform. They also correspond to the volcanoclastic levels defined in different parts of the Trans European Suture Zone in Poland.
Źródło:
Geological Quarterly; 2015, 59, 3; 473--478
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Plejstocen w profilu Kończyce (Kotlina Oświęcimska) - analiza genezy i wieku na tle schematów podziału stratygraficznego czwartorzędu
Pleistocene in the Kończyce profile (Oświęcim Basin) - sediment genesis and age analysis at the background of stratigraphic schemes of the Quaternary
Autorzy:
Wójcik, A.
Nawrocki, J.
Nita, M.
Powiązania:
https://bibliotekanauki.pl/articles/2063323.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
paleomagnetyzm
palinologia
glacjał
interglacjał
plejstocen
czwartorzęd
Kotlina Oświęcimska
palaeomagnetic investigation
pollen analysis
glacial
interglacial
Pleistocene
Quaternary
Oświęcim Basin
Opis:
W południowej części Kotliny Oświęcimskiej, na terenie żwirowni w Kończycach odsłaniają się utwory czwartorzędowe o różnej genezie. Wykonane badania pozwoliły na ich rozpoziomowanie. Stwierdzono sześć serii osadowych leżących na osadach mioceńskich. Wyróżniono dolną serię rzeczną przykrytą przez serię osadów glacigenicznych, powyżej których lokalnie stwierdzono serię dolnych mułków organicznych z florą interglacjalną, charakteryzujących się odwrotną polarnością magnetyczną. Opisana seria mułków reprezentuje fragment sukcesji ciepłego interglacjału, którą powiązano z I interglacjałem kompleksu kromerskiego. Na ściętych osadach glacigenicznych i mułkach organicznych leży górna seria rzeczna przykryta górnymi mułkami organicznymi, w obrębie których zarejestrowano granicę Brunhes-Matuyama (B/M). Bezpośrednio powyżej tej granicy, w obrębie mułków, na podstawie badań palinologicznych stwierdzono występowanie fragmentów dwóch interglacjałów rozdzielonych piętrem zimnym. Utwory reprezentujące te ciepłe odcinki plejstocenu leżą bezpośrednio powyżej granicy B/M, co pozwala je łączyć z II i III interglacjałem kromerskim. Całość przykryta jest kilkumetrową serią utworów lessopodobnych ze śladami gleb kopalnych. Osady glacigeniczne, leżące poniżej granicy B/M i utworów interglacjalnych, są starsze od kompleksu kromerskiego i nie mogą być korelowane ze zlodowaceniem Elstery lub Mindel, jak dotychczas uważano. Reprezentowane przez nie nasunięcie lądolodu należy raczej korelować z Günzem i z najstarszymi przedkromerskimi śladami zlodowaceń w Europie Zachodniej. W Polsce być może odpowiada ono zlodowaceniu podlaskiemu. W omawianym profilu mamy zatem fragmenty sukcesji trzech interglacjałów, przy czym najniższy jest starszy od granicy Brunhes-Matuyama. Sukcesja pyłkowa jest inna niż w dotychczas znanych stanowiskach interglacjalnych w Polsce. Otrzymane wyniki sugerują konieczność nieco innego niż dotychczas spojrzenia na zasięg i wiek maksymalnego nasunięcia lądolodu.
In the southern part of the Oświęcim Basin, in the area of the Kończyce quarry, the Quaternary deposits of different genesis crop out. Thanks to the performed investigations, particular horizons of these deposits have been identified. The lower fluvial series is overtopped with the glacigenic sediments. Above the latter, the lower series of organic mud with the interglacial flora occurs in places. This series is characterised by the reverse magnetic polarity. The discussed mud series represents a fragment of the warm interglacial succession and corresponds to the lst interglacial of the Cromerian Complex. The upper fluvial series overlain by an upper organic mud series, in which Brunhes-Matuyama boundary is registered, rests on the cut-off glacigenic deposits and organic muds. Directly above this boundary, in the organic muds, fragments of two interglacials separated by a cold stage have been identified by palynological methods. All the deposits are covered with the series of the loess-like sediments with the traces of the fossil soils. The glacigenic deposits occurring below the B/M boundary and interglacial sediments are older than the Cromerian Complex, and thus cannot be correlated with the Elster and Mindel glaciations as it has been accepted until now. This ice-sheet advance, in its maximum extent in southern Poland, is older and should rather be correlated with the Gunz and with the oldest, pre-Cromerian traces of glaciations in Western Europe. In Poland it might correspond to the Podlasie Glaciation. Thus, in the discussed profile there are fragments of three interglacials, and the lowermost one is older than the Brunhes-Matuyama boundary. The pollen succession differs from those known from interglacial sites in Poland. The obtained results suggest a new insight into the extent and age of the maximum ice-sheet advance than it has been accepted until now. The performed studies allow to infer that the oldest ice-sheet advance had also the largest extent in Poland. The performed study has cognitive aspects and the obtained results are a new input to the state of knowledge, thus can serves as a reference for further studies on the range of the Scandinavian Glaciation in its maximum extent. The Kończyce profile should be treated as a benchmark for the Quaternary stratigraphy of Western and Middle Europe.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2004, 409; 5-50
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Buntsandstein magnetostratigraphy from the northern part of the Holy Cross Mountains
Autorzy:
Nawrocki, J.
Kuleta, M.
Zbroja, S.
Powiązania:
https://bibliotekanauki.pl/articles/2058884.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Holy Cross Mountains
Buntsandstain
palaeomagnetic pole
magnetostratigraphy
Opis:
Lower and Middle Buntsandstein sediments from the northern part of the Holy Cross Mountains (Central Poland) were studied palaeomagnetically. The obtained palaeomagnetic pole fits well to the Early Triassic segment of the stable European apparent polar wander path. This indicates that there were no detectable horizontal tectonic rotations in this part of the Holy Cross Mountains after the Early Triassic. In the lowermost part of the Buntsandstein sequence (the A0 and A1 units) the basal Triassic normal polarity zone was identified, whereas a reversed polarity dominates in the youngest rocks of the studied sections. This predominantly reversed part can be correlated with the Pomorze Formation (lower part of the Middle Buntsandstein). The correlation of these magnetic polarity records with magnetostratigraphic data from the other parts of the Central European Basin as well as from the Tethyan sections shows that in the studied area, the Permian-Triassic boundary should be placed near the boundary between the Top Terrigenous Series (uppermost Zechstein) and the A0 unit (lowermost Buntsandstein). In the German part of the Central European Basin the Permian–Triassic boundary coincides with the boundary between the Lower and Upper Bröckelschiefer. The Buntsandstein rocks from the localities of Wióry and Sosnowica contain numerous vertebrate tracks. According to the results of magnetostratigraphic correlation they are of Dienerian (Early Triassic) age.
Źródło:
Geological Quarterly; 2003, 47, 3; 253-260
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
40Ar-39 Ar ages of selected rocks and minerals from the Kraków-Lubliniec Fault Zone, and their relation to the Paleozoic structural evolution of the Malopolska and Brunovistulian terranes (S Poland)
Autorzy:
Nawrocki, J.
Krzemiński, L.
Pańczyk, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059087.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
S Poland
late Paleozoic
palaeogeography
Ar-Ar geochronology
Opis:
New 40Ar-39 Ar isotope ages of mafic and felsic rocks from the contact zone of the Malopolska and Brunovistulian terranes are presented and discussed. A 40Ar-39 Ar age estimation of detrital muscovite from a Lower Devonian "old red" type sandstone drilled on the Malopolska side of this zone was also done. Our studies reveal that three events of Paleozoic magmatic activity took place in the study area. The oldest, late Emsian episode is recorded by a diorite from the core part of an intrusion penetrated by the Sosnowiec IG 1 borehole. A younger, Visean event is documented by a diabase cored in the borehole WB-137. Diabases from Niedwiedzia Góra and from borehole PZ-10, and a rhyodacite from borehole 16-WB gave early Permian (Artinskian-early Sakmarian) ages. The youngest, middle Sakmarian age was obtained for a diabase forming the external parts of the Sosnowiec IG 1 polycyclic intrusion. A diorite penetrated by the Sosnowiec IG 1 borehole was emplaced during the late Emsian extension that preceded the Lochkovian-Pragian? transpression related to the final docking and amalgamation of the Brunovistulian Terrane.
Źródło:
Geological Quarterly; 2010, 54, 3; 289-300
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wiek izotopowy a wiek paleomagnetyczny ryodacytów z Zalasu koło Krakowa (S Polska)
Isotope and paleomagnetic ages of the Zalas rhyodacites (S Poland
Autorzy:
Nawrocki, J.
Lewandowska, A.
Fanning, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074529.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wiek izotopowy
paleomagnetyzm
ryodacyty
perm
Polska Południowa
isotope age
paleomagnetism
rhyodacite
Permian
southern Poland
Opis:
The single-grain U-Pb dating of most zircon grains separated from the Zalas rhyodacites gave mean age of the magma emplacement 294.2 š 2.1 Ma. Some zircons, however, displayed younger ages (268.7š 3.4 Ma), probably related to metasomatic alterations of these rocks. The paleomagnetic ages of the Zalas intrusion and its metasomatosis are slightly younger. It is probably connected with a certain error of time calibration of the reference apparent polar wander path used for paleomagnetic dating.
Źródło:
Przegląd Geologiczny; 2007, 55, 6; 475-478
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stephanian-Early Permian basaltic trachyandesites from the Sławków and Nieporaz-Brodła Grabens near Kraków, Southern Poland
Autorzy:
Lewandowska, A.
Rospondek, M. J.
Nawrocki, J.
Powiązania:
https://bibliotekanauki.pl/articles/191897.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Upper Carboniferous/Permian volcanism
a-a lava flows
autoclastic breccias
basaltic trachyande-sites
transitional calc-alkaline to alkaline rocks
hydrous magma
Opis:
In the Kraków-Lubliniec section of the major Hamburg-Kraków-Dobrogea Fault Zone (HKDFZ), the Stephanian-Early Permian magmatic activity was simultaneous with subsidence/uplift of formed blocks. In the proximity of the uplifted areas the sedimentation started with fanglomerates, distally passing into playa siltstone and was accompanied by volcanism. In the Nieporaz-Brodła graben, basaltic trachyandesite a-a lava flows with autoclastic breccias reach ca. 150 m in thickness. The weathering recorded as adhesive rims around breccia clasts reflects palaeosoil formation during quiescence periods between the eruptions. The eruptions were effusive although scoriaceous lava indicates high volatile content of the magma. The water content before eruption had to be over 2 wt. percent. Only then the crystallisation model predicts accurately the type, composition and order of the crystallising phases. Thus, the basaltic trachyandesite magma originated from a source containing hydrous phase (i.e., amphibole or phlogopite). All the studied basaltic trachyandesites had fayalitic olivine on their liquidus reflecting the crystallisation stage in a magma chamber at crustal depths. During final decompression on the magma ascent due to water exsolution, the olivine was followed by plagioclase, spinel, augite, ilmenite, apatite, K-feldspar and residual high-K rhyolitic glass. The high potassium content of these volcanics was thus a primary feature reflecting the source geochemistry and differentiation trend, and its consequence was potassium metaso- matism. Due to water exsolution the glass was altered, however, homogenous interstitial glass survived in some rocks. The glass is strongly enriched in incompatible trace elements, showing that it is a highly fractionated residual melt fraction of the basaltic trachyandesite magma. Thus, the glass geochemistry reflects the trend of fractional crystallisation indicating that co-occurring K-rich felsic rocks were not derived from the same magma. All the basaltic trachyandesites studied have calc-alkaline to alkaline affinity. They contain fayalitic olivine and are low in MgO <5 wt. %, Cr and Ni, the features characteristic for evolved magmas. They show significant negative Sr/Sr*> 0.5-0.80 and small Eu/Eu* > 0.9-1.0 anomalies suggesting fractionation of plagioclase. The Eu/Eu* anomaly is probably compensated by amphibole retaining in the source. Negative Nb, Ti anomalies suggest Fe-Ti oxide fractionation characteristic for calc-alkaline evolution trend. A significant enrichment in LREE relatively to HREE (La/Yb > 10) indicates subduction-related metasomatism. However, the described tectonic context is inconsistent with subduction related characteristics. Concluding, the observed geochemical characteristics indicate remarkable role of water in magma evolution. The volcanism was related to strike-slip dextral movement along the Kraków-Lubliniec section of HKDFZ, transformed into crustal extension and subsidence, the features typical for the formation of pull-apart basins, in the late stages of the Variscan orogen evolution.
Źródło:
Annales Societatis Geologorum Poloniae; 2010, 80, No 3; 227-251
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New 40Ar-39Ar age constrains for magmatic and hydrothermal activity in the Holy Cross Mts. (southern Poland)
Autorzy:
Nawrocki, J.
Salwa, S.
Pańczyk, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060553.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Ar-Ar geochronology
diabases
mineralization
Holy Cross Mountains
Opis:
New 40Ar-39Ar isotope ages of diabase intrusions from the Holy Cross Mountains (Poland) confirm the presence of at least two events of Paleozoic magmatic activity in the study area. The oldest, latest Silurian/earliest Devonian (ca. 424–416 Ma) episode is recorded by a diabase from the Bardo Syncline (Zarobiny PIG-1 borehole) in the Kielce Region. A younger, Serpukhovian (ca. 331–323 Ma) event is documented by a diabase from the Milejowice-1 borehole drilled in the Łysogóry Region. The diabase intrusion penetrated by the Wzorki-1 borehole, also located in the Łysogóry Region, is most probably of the same age. It provided, however, consistent mid-Triassic (243 Ma) 40Ar-39Ar isotopic age reflecting its pervasive hydrothermal alteration. The first stage of the post-Caledonian hydrothermal activity in the Holy Cross Mts. which produced polymetallic copper and iron-bearing mineralisation may be linked with the younger magmatic phase defined here. The second stage of post-Caledonian hydrothermal activity in the Holy Cross Mts., associated with the lead-zinc mineralisation, may be correlated with the Middle Triassic hydrothermal event recorded in the Wzorki diabase. Suggestions of temporal relationships between magmatic/hydrothermal activities and mineralisation events should, however, be constrained by further detailed geochemical and mineralogical studies.
Źródło:
Geological Quarterly; 2013, 57, 3; 551--560
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Isotopic ages of selected magmatic rocks from King George Island (West Antarctica ) controlled by magnetostratigraphy
Autorzy:
Nawrocki, J.
Pańczyk, M.
Williams, I.
Powiązania:
https://bibliotekanauki.pl/articles/2058738.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Antarctica
King George Island
magnetostratigraphy
isotopic ages
Opis:
Isotopic and palaeomagnetic studies were carried out in the central part of King George Island. Selected mafic to intermediate igneous rocks were sampled for this purpose. Single-grain U-Pb dating of zircons from basalts to dacites was controlled by a whole rock 40Ar-39Ar data and the magnetostratigraphy. Five magmatic activity phases were distinguished in the SE coast of King George Island. The oldest, late Cretaceous (Campanian) phase represented by basalts of the Uchatka Point Formation are followed by the early to middle Eocene (~53–43 Ma) phase documented by the lava flows whose ages decrease from SW to NE. Next younger magmatic activity phases were recorded by the lava flows or vertical intrusions emplaced in the late Eocene (~37–35 Ma), late Oligocene (~~28-25 Ma) and late Pliocene to Holocene. The early to middle Eocene magmatic activity phase was the most extensive, producing the largest volume of magma in the study area. The new age determinations allow a more precise and credible stratigraphic correlation of the interbeds of sedimentary rocks observed in some places within the magmatic succession. The glacial provenance of the Herv' Cove diamictite is not obvious. It might represent a mountain river environment. Intense volcanic activity could be additional factor modelling the climate conditions of Antarctica in Paleogene
Źródło:
Geological Quarterly; 2011, 55, 4; 301-322
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palaeomagnetic studies of the loess-palaeosol sequence from the Kolodiiv section (East Carpathian Foreland, Ukraine)
Autorzy:
Nawrocki, J.
Boguckyj, A.
Łanczont, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059494.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Ukraine
Kolodiiv
loess
Upper Pleistocene
palaeomagnetism
Opis:
The Upper Pleistocene loess-palaeosol sequence from the Kolodiiv section (East Carpathian Fore land) has been palaeomagnetically studied. Almost all samples displayed moderate to high positive palaeomagnetic inclinations and declinations en closed between 320° and 40°. How ever, one sample from the fossil soil of the last inter glacial pedocomplex (at 16.6 m pro file depth) was reverse magnetized and there fore can be correlated with the Blake Palaeomagnetic Event. Consequently that palaeosol can be related to (Oxygen Isotope Stage) OIS 5e1. An other sample from the Dubno 1 interstadial palaeosol demonstrated southern declination and significant lowering of inclination (up to 40°). This might be a record of the Laschamp Palaeomagnetic Event or of any Late Pleistocene palaeomagnetic excursion. The magnetic susceptibility and anhysteretic remanent magnetization data reflect the presence of several soils forming during the warm conditions of OIS 5 and the complex nature of the Eemian warming. Two palaeosols that developed between ca.115 ka and 120 ka indicate at least two climatic optima during the Eemian. High values of magnetic susceptibility (up to 300 Ą 10-6 SI units) noted in the middle of the section that contains slump deposits (9.5 m to 11m of depth) suggest that this material was derived from older soils of inter glacial type.
Źródło:
Geological Quarterly; 2007, 51, 2; 161-166
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A Carboniferous/Permian, calc-alkaline, I-type granodiorite from the Małopolska Block, Southern Poland: implications from geo chemi cal and U-Pb zircon age data
Autorzy:
Żelaźniewicz, A.
Pańczyk, M.
Nawrocki, J.
Fanning, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059094.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Brunovistulian
Upper Silesian Block
Kraków-Lubliniec fault zone
SHRIMP
Variscan foreland
strike-slip
Opis:
A granodiorite from bore hole WB-102A in the Dol ina Będkowska, the Małopolska Block (MB), South ern Po land, yielded a mean U-Pb zir con age of 300 š3 Ma with SHRIMP II. No in her ited older com po nent was de tected. Geo chemically, it is a K-rich, I-type, calc-al ka line granodiorite with su pra-subduction char ac ter is tics (neg a tive Nb and Ti anom a lies). Silicic ig ne ous rocks are abun dant at the MB mar gin along the Kraków-Lubliniec Fault Zone (KLFZ) across which it ad joins to the Up per Silesian Block (USB) where such rocks are scarce. Both blocks be long to the Variscan fore land. Gra nitic rocks can not, how ever, gen er ate at fore land set tings. Thus, the hy poth e sis is put for ward that the par ent melt for the silicic rocks was de rived from the thick ened lower crust of the Variscan orogenic belt ow ing to extensional de com pres sion melt ing, and trans ported away to wards pul-apart open ings de vel oped along the crustal-scale fault zone (KLFZ) that un der went a com plex strike-slip his tory around the Car bon if er ous/Perm ian bound ary.
Źródło:
Geological Quarterly; 2008, 52, 4; 301-301
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geophysical cartography in Poland : an overview
Autorzy:
Krzywiec, P.
Nawrocki, J.
Polechońska, O.
Wróblewska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2065895.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geophysical cartography
seismic data
magnetic field
gravity field
thermal field
petrophysical parameters
Opis:
Regional analysis and mapping of various geophysical data has been recognized as an important — even crucial — element of geological studies for many years. Due to rapid development of advanced numerical tools it is presently possible to construct, maintain and comprehensively analyse even very large geo-databases, including seismic, gravity, magnetic, geothermal and other geophysical data. In many countries, national geological surveys, commercial companies and research institutions are involved in mapping projects focused on spatial representation of geophysical data that could later be used for various studies. Recently, new policy of the Polish Ministry of Environment regarding geological cartography in years 2005–2020 has been declared (cf. Ber & Jezierski, 2004). In this document, geological cartography is used as a rather wide term that includes also other geo-disciplines like geoenvironmental studies or surface geochemistry. Among them, mapping of geophysical data is also mentioned. In this paper, short overview of the current state-of-the-art of selected aspects of regional geophysical mapping in Poland is given, with some remarks regarding potential directions of future work.
Źródło:
Przegląd Geologiczny; 2005, 53, 10/2; 967-972
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Weeds in potato culture and their outcome in spreading of Alternaria spp.
Autorzy:
Kurzawińska, H.
Mazur, S.
Nadziakiewicz, M.
Nawrocki, J.
Powiązania:
https://bibliotekanauki.pl/articles/11876809.pdf
Data publikacji:
2018
Wydawca:
Uniwersytet Przyrodniczy w Lublinie. Wydawnictwo Uniwersytetu Przyrodniczego w Lublinie
Opis:
The aim of this study was to determine whether the weeds accompanying potato crops can be a source of Alternaria spp. causing Alternaria leaf blight and to determine the genetic similarities of Alternaria alternata isolates infecting selected weeds: Chenopodium album, Cirsium arvense and tested potato cultivar. Three-year field experiment was conducted on the potato cultivar ‘Vineta N’. The isolates were classified into different species on the basis of macro- and microscopic features. In each year of the study, A. alternata dominated among the isolated fungi colonizing the leaves of potato plants and the selected weeds. The genetic similarities of A. alternata isolates was determined by the RAPD-PCR method. Tested genetic forms of A. alternata were closely related; only small differences in the pattern of the separated amplification products was evidenced. The dominance of A. alternata on the weeds accompanying potato crops suggests that if weed infestation is extensive, the pathogen is very likely to spread and its population to increase.
Źródło:
Acta Scientiarum Polonorum. Hortorum Cultus; 2018, 17, 6; 159-166
1644-0692
Pojawia się w:
Acta Scientiarum Polonorum. Hortorum Cultus
Dostawca treści:
Biblioteka Nauki
Artykuł
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