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pro vyhledávání: '"Paweł Brański"'
Autor:
Stanisław Z. Mikulski, Paweł Brański, Rafał Małek, Andrzej Chmielewski, Grzegorz Pieńkowski, Karol Zglinicki
Publikováno v:
Przegląd Geologiczny. 69:379-385
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 101:421-472
A multidisciplinary study of the Devonian–Carboniferous boundary interval in pelagic successions of the Holy Cross Mountains and Sudetes and the ramp successions in the Western Pomerania region (Poland) is presented herein. The analysis applies the
Autor:
Paweł Brański
Publikováno v:
Biuletyn Państwowego Instytutu Geologicznego. 472:255-270
PRELIMINARY CHARACTERISTICS OF RARE EARTH ELEMENTS AND OTHER TRACE ELEMENTS IN FINE-GRAINED DEPOSITS FROM THE TRIASSIC-JURASSIC TRANSITION IN THE FORMER MID-POLISH TROUGH Fine-grained siliciclastic rocks from the Triassic-Jurassic transition (Rhaetia
Autor:
Paweł Brański, Stanisław Z. Mikulski
Publikováno v:
Geological Quarterly.
Nineteen samples of uppermost Triassic and Lower Jurassic claystones and mudstones, which were formed in the epicontinental Polish Basin, were analysed by inductively coupled plasma mass spectrometry (ICP-MS) for rare earth elements (REE) and other s
Autor:
Paweł Brański, Marek Dulinski, Mirosław Kobierski, Adam Postawa, Hanna Jaworska, Anna Zurek, Przemysław Wachniew
Publikováno v:
Geological Quarterly. 58
The Triassic-Jurassic boundary interval (ca. 201 Ma) was a time of sudden global environmental changes triggered by Pangea breakup and Central Atlantic Magmatic Province (CAMP) development. The bulk-rock mineralogy, clay mineralogy and major element
Eight climatic events can be distinguished in the Triassic–Jurassic (ca. 201 Ma) continental strata of Poland. These events are distinguished by kaolinite/illite ratio, chemical index of alteration (CIA), color of sediments, and palynomorphs. The f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ec341fc77baac67fca90c7393ff631a
https://doi.org/10.1130/2014.2505(13)
https://doi.org/10.1130/2014.2505(13)