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    Wyświetlanie 1-5 z 5
    Tytuł:
    Population diversity in ant-inspired optimization algorithms
    Autorzy:
    Byrski, Aleksander
    Węgrzyński, Krzysztof
    Radwański, Wojciech
    Starzec, Grażyna
    Starzec, Mateusz
    Bargiel, Monika
    Urbańczyk, Aleksandra
    Kisiel-Dorohinicki, Marek
    Powiązania:
    https://bibliotekanauki.pl/articles/2097962.pdf
    Data publikacji:
    2021
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    ant colony optimization
    diversity measuring
    exploitation and exploration balance
    metaheuristics
    Opis:
    Measuring the diversity in evolutionary algorithms that work in real-value search spaces is often computationally complex, but it is feasible; however, measuring the diversity in combinatorial domains is practically impossible. Nevertheless, in this paper we propose several practical and feasible diversitymeasurement techniques that are dedicated to ant colony optimization algorithms, leveraging the fact that we can focus on a pheromone table even though an analysis of the search space is at least an NP problem where the direct outcomes of the search are expressed and can be analyzed. Besides sketching out the algorithms, we apply them to several benchmark problems and discuss their efficacy.
    Źródło:
    Computer Science; 2021, 22 (3); 297-320
    1508-2806
    2300-7036
    Pojawia się w:
    Computer Science
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB)
    Autorzy:
    Golonka, Jan
    Krobicki, Michał
    Wendorff, Marek
    Starzec, Krzysztof
    Siemińska, Aneta
    Olszewska, Barbara
    Wierzbowski, Andrzej
    Oszczypko, Nestor
    Salata, Dorota
    Tyszka, Jarosław
    Uchman, Alfred
    Sidorczuk, Magdalena
    Aubrecht, Roman
    Skupien, Petr
    Vašíček, Zdeněk
    Kowal-Kasprzyk, Justyna
    Waśkowska, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/27323884.pdf
    Data publikacji:
    2023
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Źródło:
    Geotourism / Geoturystyka; 2023, 3-4 (74-75); 5-70
    1731-0830
    Pojawia się w:
    Geotourism / Geoturystyka
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Permian versus Jurassic geotectonic position of the Lhasa block – facts and controversies
    Autorzy:
    Krobicki, Michał
    Golonka, Jan
    Starzec, Krzysztof
    Iwańczuk, Joanna
    Powiązania:
    https://bibliotekanauki.pl/articles/24202131.pdf
    Data publikacji:
    2023
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    Permian
    Jurassic
    geotectonics
    Opis:
    The Cimmerian Continent (or Cimmeria, Cimmerian terrane, Cimmerian blocks) was detached from eastern Gondwana in the Late Paleozoic as a sliver/ribbon of continental strip rifting elements. Recently, these elements belong to an almost continuous long belt (ca. 13,800 km) from central Italy trough Greece, Turkey, Iran, Afghanistan, Tibet, SW China, Myanmar, Thailand up to Indonesia (Sumatra). The palaeogeographic position and relationship of some elements during Permian-Mesozoic times is still matter of discussion. The Qiangtang and Lhasa blocks (present-day Tibet) belong to these elements and their location in space and time and their relationship causes a lot of controversies. Their position alongside eastern Gondwana in the mid-Early Permian (ca. 290–285 Ma) are suggested both by palaeomagnetic and facies studies. Palaeomagnetic studies indicated this position one decade ago, which has been confirmed by recent studies. The Cimmerian Continent [Iran (Alborz)-Qiangtang-Baoshan-Tengchong-Sibumasu] was separated from the Gondwanian part of Pangea during mid-Early Permian time by rifting and drifting. Northwards migration of it took place during Permian-Triassic times caused wide opening of the Bangong‐Nujiang Tethyan Ocean and closing of the Paleotethys Ocean but the Lhasa block was still southern margin of the Bangong‐Nujiang Ocean. The Triassic Indosinian Orogeny has been one of the most spectacular geotectonic event reflecting collision of this continent with Indochina block and closure of the Paleotethys Ocean. The separation of the Lhasa block from Gondwana is enigmatic but most probably took place during earliest Jurassic times. This separation was followed by quick shift northward. Intensive sedimentological studies of the Late Triassic (Carnian-Norian) several flysch-type turbidites in the eastern Tethyan Himalaya (e.g. Qulonggongba, Pane Chaung, Langjiexue, Quehala, Duoburi formations/groups) indicate that their provenance was connected with Lhasa block, which has been their source area during early-stage evolution of the Neotethys. The late Early Permian rift-related basaltic magmatism in northern Baoshan (in SW China) and sourrounding regions was connected with first step of separation from Gondwana margin of this block (together with South Qiangtang and Sibumasu blocks and simultaneously with opening of the Bangong‐Nujiang Ocean before the Middle Permian)  – independently of Lhasa block which was separated later, the most probably during Late Triassic or Triassic/Jurassic transition time with very wide space of the Bangong‐Nujiang Tethyan Ocean between Qiangtang and Lhasa blocks (2,600 km ±710 km  – 23.4° ±6.4° during the Middle Jurassic with its maximum width in the Late Triassic). From the palaeobiogeographic point of view, the worldwide distribution of Pliensbachian-Early Toarcian large bivalves of the so-called Lithiotis-facies, dominated by Lithiotis, Cochlearites, Litioperna genera revealed by the authors’ studies, indicates very rapid expansion of such type of bivalves alongside southern margin of Neotethys, and could be good evidence of palaeogeographic position of the Lhasa block in this time. Himalayan and Tibetan (Nyalam area) occurrences of Lithiotis and/or Cochlearites bivalves could help to place the Lhasa block nearby the Gondwana during Early Jurassic times. This palaeobiogeographic research contradict another interpretation based on different fossils (Permian fusulinids and brachiopods) interpreted as subtropical fauna, which could occur in low subtropical latitudes together with other parts of the Cimmerian Continent.
    Źródło:
    Geotourism / Geoturystyka; 2023, 1-2 (72-73); 38--38
    1731-0830
    Pojawia się w:
    Geotourism / Geoturystyka
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Campanian-Paleocene Jaworzynka Formation in its type area (Magura Nappe, Outer Carpathians)
    Autorzy:
    Waśkowska, Anna
    Golonka, Jan
    Starzec, Krzysztof
    Cieszkowski, Marek
    Powiązania:
    https://bibliotekanauki.pl/articles/1835592.pdf
    Data publikacji:
    2020
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Upper Cretaceous
    Paleogene
    lithostratigraphy
    foraminifera
    biostratigraphy
    kreda górna
    paleogen
    litostratygrafia
    otwornice
    biostratygrafia
    Opis:
    The Campanian-Paleocene Jaworzynka Formation, a part of the Magura Nappe succession in the Polish Outer Carpathians, is described in terms of its detailed litho- and biostratigraphy. The formation stretches along the marginal part of the Siary Unit, from the Jaworzynka stratotype area in the Silesian Beskid Mts up to the Mszana Dolna area in the Beskid Wyspowy Mts. Its equivalent in the Moravskoslezské Beskydy Mts of the Czech Republic is the Soláň Formation. In the stratotype area, the formation displays complex structure. We distinguish four lithological units, i.e., Biotite Sandstone and Shale (I), Shale (II), Mutne Sandstone Member (III) and Thin-bedded Turbidite (IV) and provide the first detailed biostratigraphy of particular units. The first unit forms the most prominent part of the formation. It was deposited in the Middle Campanian-earliest Maastrichtian within the upper part of Caudammina gigantea Zone up to the lower part of the Rzehakina inclusa Zone. The second unit occurs only locally and its age is limited to the Maastrichtian, to the Rzehakina inclusa Zone. The third unit is composed of thick-bedded sandstones that in some parts may form more than the half of the total thickness of the formation. It is Late Maastrichtian-Danian in age and is placed in the upper part of the Rzehakina inclusa Zone and the lower part of the Rzehakina fissistomata Zone. It is usually covered by a thin package of thin-bedded turbiditic sandstone and shales of Danian-Thanetian age with foraminifera of the Rzehakina fissistomata Zone.
    Źródło:
    Acta Geologica Polonica; 2021, 71, 3; 345-370
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dzieje Oddziału Krakowskiego Polskiego Towarzystwa Geologicznego
    History of the Kraków Branch of the Polish Geological Society
    Autorzy:
    Waśkowska, Anna
    Sikora, Rafał
    Starzec, Krzysztof
    Ślączka, Andrzej
    Powiązania:
    https://bibliotekanauki.pl/articles/2074316.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Krakowski Oddział PGS
    historia nauk geologicznych
    Polskie Towarzystwo Geologiczne
    Kraków Branch of the PGS
    history of geological science
    Polish Geological Society
    Opis:
    The Kraków Branch of the Polish Geological Society (PGS) was established in 1922 and is the oldest and largest regional branch of the PGS. Initially, it was managed directly by the PGS Main Board, and from 1963, it has its own board. From the beginning, it has been one of the most active centres of the PGS and supported the work of the PGS management board in organizational activities in the country and in foreign cooperation. During World War II, its members gave secret lectures, and in the post-war period, they took part in reactivating the PGS activities and establishing both other branches and most of the specialist sections of PGS. The branch organized about 30% of all annual PGS Scientific Meetings and several dozen other scientific symposia and popular scientific sessions. It was the centre to initiate the organization of Polish Geological Congresses in the 21st century. The Kraków Branch includes representatives of all scientific institutes from Kraków and beyond, dealing with Earth sciences.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 4; 292--299
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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