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Wyszukujesz frazę "Western part" wg kryterium: Temat


Wyświetlanie 1-6 z 6
Tytuł:
The site of western ragweed (Ambrosia psilostachya DC.) in the western part of Szczecin Lowland
Stanowisko ambrozji zachodniej (Ambrosia psilostachya DC.) w zachodniej części Niziny Szczecińskiej
Autorzy:
Kutyna, I.
Mlynkowiak, E.
Lesnik, T.
Powiązania:
https://bibliotekanauki.pl/articles/82822.pdf
Data publikacji:
2014
Wydawca:
Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
Tematy:
Western ragweed
ragweed
Ambrosia psilostachya
locality
cover coefficient
Diantho-Armerietum elongatae complex
invasive species
phytosociological stability
Western part
Szczecin Lowland
Opis:
Ambrozja zachodnia (Ambrosia psilostachya DC.) jest gatunkiem inwazyjnym notowanym w Polsce na nielicznych stanowiskach. W zachodniej części Niziny Szczecińskiej jest to 3 stanowisko. Zbiorowisko z ambrozją zachodnią występuje na poboczu dwupasmowej drogi Berlin–Szczecin–Chociwel na glebie wytworzonej z piasków (słabogliniastego i gliniastego lekkiego) przesuszonych, nieco zasolonych, o odczynie obojętnym, z niewielką zawartością próchnicy i CaCO3 (od 3 do 5%). Na podstawie 9 zdjęć fitosocjologicznych fitocenozy z obecnością tego gatunku zaliczono do zespołu Diantho-Armerietum elongatae z wyraźną tendencją nawiązującą do zbiorowiska z rzędu Arrhenatheretalia, z racji znacznego udziału w nim gatunków zbiorowisk seminaturalnych – Festuca rubra (S = V, D = 3000) i Arrhenatherum elatius (S = IV, D = 750). Ambrozja zachodnia jest stałym składnikiem fitocenoz (S = V), osiągając w nich znaczne pokrycie (D = 3139).
Western ragweed (Ambrosia psilostachya DC.) is an invasive species recorded in Poland in few sites. In the area of western Szczecin Lowland it is the 3rd site. The community with ragweed occurs on the roadside of a two-lane Berlin–Szczecin–Chociwel highway on soil formed by sands (slightly loamy and light loamy), desiccated, slightly salinized, with neutral pH, and with low content of humus and CaCO3 (from 3 to 5%). On the basis of 9 phytosociological relevés, phytocoenoses with its presence were classified as Diantho-Armerietum elongatae with a clear tendency connected to the community of Arrhenatheretalia, due to a significant share of semi-natural communities species such as Festuca rubra (S = V, D = 3000) and Arrhenatherum elatius (S = IV, D = 750). Western ragweed is a regular constituent of phytocoenoses (S = V) and it reaches a significant coverage in them (D = 3139).
Źródło:
Folia Pomeranae Universitatis Technologiae Stetinensis. Agricultura, Alimentaria, Piscaria et Zootechnica; 2014, 32
2081-1284
Pojawia się w:
Folia Pomeranae Universitatis Technologiae Stetinensis. Agricultura, Alimentaria, Piscaria et Zootechnica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmiany średniej refleksyjności witrynitu uwęglonej materii organicznej w warstwach istebniańskich jako przykład tektonicznej ewolucji płaszczowiny śląskiej (zachodnie Karpaty fliszowe)
Changes of random vitrinite reflectance of coalified organic matter in the Istebna Beds as evidence of tectonic evolution of the Silesian nappe (western flysch Carpathians)
Autorzy:
Syrek, M.
Powiązania:
https://bibliotekanauki.pl/articles/183425.pdf
Data publikacji:
2009
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Zewnętrzne Karpaty Zachodnie
płaszczowina śląska
warstwy istebniańskie
uwęglona materia organiczna
średnia refleksyjność witrynitu
western part of Outer Carpathians
Silesian unit
Istebna beds
coalified organic matter
random vitrinite reflectance
Opis:
Organic matter in the Istebna beds occur as dark laminas in sandy mudstones. Coalification degree of organic matter in the Istebna beds is related with orogenic period of the flysch Carpathians. There is no correlation with age of rocks and subsidence processing started during Paleogene. Higher values of vitrinite reflectance in southern part of Silesian Unit have been noticed.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2009, 35, 2/1; 61-68
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrothermal ore mineralization from the Polish part of the Tatra Mts., Central Western Carpathians
Autorzy:
Sitarz, Magdalena
Gołębiowska, Bożena
Nejbert, Krzysztof
Dimitrova, Dimitrina
Milovský, Ratislav
Powiązania:
https://bibliotekanauki.pl/articles/2055847.pdf
Data publikacji:
2021
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
tetrahedrite
hydrotherma ore mineralization
fluid inclusions
LA-ICP-MS study
Tatric Superunit
Polish part of the Western Tatra Mts.
Polska
Opis:
Several areas with hydrothermal ore mineralization are present in the Polish part of the Western Tatra Mts. Massive and disseminated sulfides, mainly minerals from the tetrahedrite group and chalcopyrite, fill quartz veins accompanied by siderite, dolomite and baryte – many of these were mined between the 16th and 18th century. This paper presents information on the mineralogy of the common sulfides and the preliminary studies of both the isotopic composition of sulfur in tetrahedrite as well as the origin of hydrothermal fluids. The most common primary sulfide minerals in the ores are tetrahedrite-(Zn) and tetrahedrite-(Fe) corresponding to Zn ranges from 1.83 to 5.87 wt.% (0.47–1.44 apfu), and Fe from 1.63 to 5.05 wt.% (0.48–1.52 apfu). The substitution of As for Sb shows maximum As content of 7.25 wt.% (1.588 apfu) which corresponds to the Sb/(Sb+As) = 0.60. Both varieties show substitutions of Bi and Hg, up 0.6 wt.% (0.049 apfu) and 0.96 wt.% (0.081 apfu), respectively, and content of trace elements: Co (max. 976 ppm), Cd (max. 735 ppm), In (max. 14 ppm). Chalcopyrite, pyrite, and galena show compositions close to the ideal formula. Differences in the content of trace elements in the studied tetrahedrite and chalcopyrite were explained by element partitioning between these minerals. The distributions of In, Ga and Sn in the studied minerals indicate that the mineralization was formed at low temperature and pressure. The homogenization temperature of the primary inclusions in quartz in the range of 120–174°C indicate the origin of mineralization in low temperature stage from low salinity fluids (up to 17.92 wt.% NaCl eq.). Stable δ34S isotopes in minerals of the tetrahedrite group suggest that the igneous fluids might be one of the sources from which ores were crystallized.
Źródło:
Geology, Geophysics and Environment; 2021, 47, 3; 159--179
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Remarks on the correlation of tectonic blocks in the foreland of the East European Craton in Poland with those in Ukraine
Autorzy:
Mizerski, W.
Stupka, O.
Olczak-Dusseldorp, I.
Powiązania:
https://bibliotekanauki.pl/articles/2060196.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
marginal part of the East-European Craton
Holy Cross Mountains
Western Ukraine
tectonics
geotectonic evolution
Opis:
According to common interpretations, two narrow crustal blocks are supposed to occur on the south-western edge or in the foreland of the East European Craton. The first one, bounded on the NE by the Nowe Miasto-Radom-Rava Ruska fault system, and on the SW by the Holy Cross Fault, stretches NW-SE from the Łysogóry-Radom region in Poland to the Rava Ruska Zone in Ukraine. The second one, bounded on the NE by the Holy Cross Fault, and from the SW by the Chmielnik-Ryszkowa Wola–Krakovets fault zone, is thought to tie together the Kielce area of the Holy Cross region with the Kokhanivka Zone in Ukraine. Both these blocks may have formed in connection with the development of regional listric faults during Precambrian asymmetric stretching of the Baltica continent, and were part of the marginal zone of the East European Craton. The sedimentary development of the blocks can be comparable to the Blake Plateau off the Florida coast. Both the Paleozoic sections and tectonic deformation styles in the Polish and Ukrainian segments of these blocks are different. Paleozoic tectonic structures of the Holy Cross region have a southern vergence, while the Paleozoic rocks of the Rava Ruska and Kokhanivka regions in western Ukraine are thrust towards the NE. This demonstrates the different tectonic evolution of the Paleozoic succession between the Holy Cross region and western Ukraine, and makes questionable the genetic relationships between these two regions. In this situation, the tectonic blocks of the foreland should be considered heterogeneous. Structural-facies evidence suggests that the SW boundary of the East European Craton should be moved at least to the Chmielnik–Ryszkowa Wola-Krakovets fault.
Źródło:
Geological Quarterly; 2016, 60, 1; 124--132
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
THE ESSENTIAL CONNECTION BETWEEN COMMON SENSE PHILOSOPHY AND LEADERSHIP EXCELLENCE
Autorzy:
Redpath, Peter A.
Powiązania:
https://bibliotekanauki.pl/articles/507500.pdf
Data publikacji:
2014
Wydawca:
International Étienne Gilson Society
Tematy:
aim
analogy
anarchy
art
body of knowledge
cause
common sense
communication
comprehensive understanding
concept
contrary
contrariety
culture
demonstration
demonstrative
equality
emotion
end
excellence
existence
explanation
fear
genus
habit
happiness
harmony
hierarchically ordered
history
hope
human
humanist
inequality
judgment
knowledge
language
leadership
logic
mathematics
memory
metaphysics
multitude
nature
operational
opposite
order
part
person
philosophy
physical
poetry
principle
quality
reason
receptivity
relationship
renaissance
resistance
rhetoric
science
soul
species
strength
syllogism
system
truth
West
Western civilization
unity
universe
virtue
whole
wonder
Opis:
This article argues that, strictly speaking, from its inception with the ancient Greeks and for all time, philosophy and science are identical and consist in an essential relationship between a specific type of understanding of the human person as possessed of an intellectual soul capable of being habituated and a psychologically-independent composite whole, or organization. It maintains, further, that absence of either one of the extremes of this essential relationship cannot be philosophy/science and, if mistaken for such and applied to the workings of cultural institutions, will generate anarchy within human culture and make leadership excellence impossible to achieve. Finally, it argues that only a return to this “common sense” understanding of philosophy can generate the leadership excellence that can save the West from its current state of cultural and civilizational anarchy.
Źródło:
Studia Gilsoniana; 2014, 3: supplement; 605-617
2300-0066
Pojawia się w:
Studia Gilsoniana
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
THE NATURE OF COMMON SENSE AND HOW WE CAN USE COMMON SENSE TO RENEW THE WEST
Autorzy:
Redpath, Peter A.
Powiązania:
https://bibliotekanauki.pl/articles/507346.pdf
Data publikacji:
2014
Wydawca:
International Étienne Gilson Society
Tematy:
aim
analogy
anarchy
art
body of knowledge
cause
common sense
communication
comprehensive understanding
concept
contemporary
contrary
contrariety
culture
demonstration
demonstrative
disorder
education
equality
emotion
end
enlightened
enlightenment
excellence
existence
explanation
fear
fundamentalistic
genus
God
habit
happiness
harmony
hierarchically ordered
history
hope
human
humanist
inequality
inspiration
inspired
judgment
justice
knowledge
language
leadership
logic
mathematics
memory
metaphysics
modern
multitude
nature
Nietzschean
operational
opposite
order
part
person
philosophy
physical
poetry
power
principle
provocative thought
quality
reality
reason
receptivity
relationship
renaissance
resistance
rhetoric
science
scientism
skeptic
sophist
soul
species
strength
success
system
truth
utopian
West
Western civilization
unity
universe
values
virtue
whole
will
wisdom
wonder
World War
Opis:
Since most pressing today on a global scale is to be able to unite religion, philosophy, and science into parts of a coherent civilizational whole, and since the ability to unite a multitude into parts of a coherent whole essentially requires understanding the natures of the things and the way they can or cannot be essentially related, this paper chiefly considers precisely why the modern world has been unable to effect this union. In so doing, it argues that the chief cause of this inability to unite these cultural natures has been because the contemporary world, and the West especially, has lost its understanding of philosophy and science and has intentionally divorced from essential connection to wisdom. Finally, it proposes a common sense way properly to understand these natures, reunite them to wisdom, and revive Western and global civilization.
Źródło:
Studia Gilsoniana; 2014, 3: supplement; 455-484
2300-0066
Pojawia się w:
Studia Gilsoniana
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-6 z 6

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