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Wyszukujesz frazę "Palaeozoic Platform" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Relative secular variations of the Earth’s magnetic field in the years1966–2016 along the profile across the main tectonic units of Poland (Zgorzelec-Wiżajny profile)
Autorzy:
Wojas, Anna
Grabowska, Teresa
Powiązania:
https://bibliotekanauki.pl/articles/184271.pdf
Data publikacji:
2019
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
relative local secular variations
geomagnetic field
total magnetic intensity
Palaeozoic Platform
Trans-European Suture Zone
East European Craton
Polska
Opis:
The paper summarizes 50 years of research on relative local secular variations of the total magnetic intensity (TMI) along Zgorzelec-Wiżajny profile (Z-W profile) through the years 1966–2016. The Z-W profile (approximately 650 km length) cuts through Europe’s major tectonic units, including a zone of Variscan folds in the Paleozoic platform (PP), the Trans-European Suture Zone (TESZ) and the Polish part of the East European Craton (EEC). Measurements of TMI were made at 31 sites of the profile and reduced to the base recordings at the Central Geophysical Observatory in Belsk. Based on linear approximations of relative geomagnetic field values changes in time, relative annual changes in time (relative secular variations) expressed in nanoteslas [nT] per year were calculated. The study on relative geomagnetic field values revealed slower secular variations of the geomagnetic field in EEC as compared to those in PP and TESZ. However, they show lower amplitudes of these variations. An interesting phenomenon are rapid changes in the time of the relative values (trends) of TMI starting from the year 2000, also expressed as the relative secular variations per year, particularly visible in PP area. In the qualitative sense, relative secular variations show a correlation with the main geological units in the Polish territory and also important elements in the seismic and geothermal model of the lithosphere.
Źródło:
Geology, Geophysics and Environment; 2019, 45, 3; 183-194
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
O nowych rozwiązaniach tektonicznych w „Atlasie geologicznym Polski”
On the new tectonic solutions in “Geological Atlas of Poland”
Autorzy:
Aleksandrowski, P.
Mazur, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075682.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Kraton wschodnioeuropejski
platforma paleozoiczna
orogen waryscyjski
strefa Teisseyre-Tornquist
zapadlisko kaledońskie
terrany
TESZ
architektura crustalna
dane sejsmiczne
dane grawitacyjne
dane magnetyczne
East European Craton
Palaeozoic Platform
Variscan Orogen
Teisseyre-Tornquist Zone
Caledonian Foredeep
terranes
crustal architecture
seismic data
gravity data
magnetic data
Opis:
Authorial comprehensive comments and explanations are given to some of the interpretations applied in the tectonic part of the newly published Geological Atlas of Poland (Nawrocki, Becker, 2017) that considerably change the hitherto generally accepted concepts. It should be, however, admitted that most of those "new’" solutions were already proposed in the past by other workers as hypotheses that could not have been tested in the then state of knowledge on Poland’s deep geology and scientific tools at hand. This has now changed with abundant new data obtained with modern seismic techniques and advanced methods of potential field modelling. Using those data, we justify the reasons for, among others, a significant eastward shifting the front of the Variscan Orogen in Poland andfor the accompanying change in position of the division line between the Precambrian and Palaeozoic platforms. We also show the rationale for accepting a far-reaching southwestward extent of the East European Craton’s crystalline basement below the Palaeozoic Platform and for reinterpretation of the Teisseyre-Tornquist Zone’s nature, together with the question of early Palaeozoic terranes in the TESZ and the situation of the Caledonian foredeep at the SW margin of the East-European Craton.
Źródło:
Przegląd Geologiczny; 2017, 65, 12; 1499--1510
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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