Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Beata Marciniak-Maliszewska"'
Autor:
Janusz Recław, Paula Sierpień, Jakub Karasiński, George Kamenov, Wayne Powell, Beata Marciniak-Maliszewska, Maciej Kałaska
Publikováno v:
Heritage Science, Vol 12, Iss 1, Pp 1-18 (2024)
Abstract This study identifies the lead ores used to produce lead artifacts used by the Romans between the first and eighth centuries AD during the construction of the fort and then the town of Novae (N. Bulgaria). For this purpose, lead samples were
Externí odkaz:
https://doaj.org/article/3d236a69baf447c9bb2d527fd2127d35
Publikováno v:
Minerals, Vol 10, Iss 2, p 190 (2020)
Na-Cu carbonates are relatively rare secondary minerals in weathering zones of ore deposits. Hereby we describe mineral composition and crystal chemistry of the most important secondary (Na)Cu minerals and their Na- and Mg-bearing associates forming
Externí odkaz:
https://doaj.org/article/d6a21df540144ef5b15a452e53980848
Autor:
Jan Środoń, Lynda Williams, Marek Szczerba, Tatiana Zaitseva, Maciej J. Bojanowski, Beata Marciniak-Maliszewska, Artur Kuligiewicz, Krzysztof Starzec, Zuzanna Ciesielska, Mariusz Paszkowski
Publikováno v:
Geochimica et Cosmochimica Acta. 352:157-174
Autor:
Anna Sałacińska, Ianko Gerdjikov, Alexandre Kounov, David Chew, Krzysztof Szopa, Ashley Gumsley, Izabela Kocjan, Beata Marciniak-Maliszewska, Foteini Drakou
Publikováno v:
Gondwana Research. 109:253-273
Publikováno v:
Mineralogical Magazine. 86:929-939
The recently defined arctite supergroup contains nine mineral members defined as hexagonal intercalated antiperovskites, most of which have been found in pyrometamorphic rocks of the Hatrurim Complex, Israel. Three members of this supergroup: nabimus
Autor:
Anna Gumsley, Krzysztof Szopa, David Chew, Ianko Gerdjikov, Petras Jokubauskas, Beata Marciniak-Maliszewska, Foteini Drakou
Publikováno v:
Lithos. :107186
Dolomite and magnesite are particularly abundant in the Precambrian strata, which is often explained by abnormal ocean chemistry favoring formation of these minerals in oceanic basins over other carbonates and Ca-sulfates. However, interpretation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f5ad7bee8afe7d4901f1a65daddd29b
https://doi.org/10.5194/egusphere-egu22-9860
https://doi.org/10.5194/egusphere-egu22-9860
Autor:
Maciej Fitt, Jakub Ciazela, Magdalena Laban, Marta Prell, Konrad Blutstein, Beata Marciniak-Maliszewska, Ewa Slaby, Leszek Latacz, Dariusz Marciniak, Marine Paquet, Marta Ciazela
Publikováno v:
Goldschmidt2022 abstracts.
Autor:
Beata Marciniak-Maliszewska, Magdalena Goryl, Maciej J. Bojanowski, Jan Środoń, Barbara Kremer, Leszek Marynowski
Publikováno v:
Geology. 48:62-66
Ediacaran siderite-bearing sedimentary rocks from the western part of the East European craton exhibit features typical of redoximorphic paleosols, including pedogenic siderite (e.g., sphaerosiderite) with uniform and negative δ18O and highly variab
Publikováno v:
Precambrian Research. 365:106379
The Ediacaran sedimentary rocks on the East European Craton (EEC) comprise chiefly siliciclastic deposits of the Volyn and Valdai series that have commonly been regarded as deposits in a shallow epicontinental sea on Baltica. However, an intermittent