The ferromanganese crusts (FMC) and nodules at Stankowa Skała near Nowy Targ (Pieniny Klippen Belt, Poland) are developed in pelagic condensed limestones. The crusts appear on an uneven surface of limestones with thinshe...
The ammonite succession in the stratigraphical interval from the Bifurcatus Zone, through the Hypselum Zone, up to the lower part of the Bimammatum Zone corresponding to a large part of the Submediterranean Upper Oxfordi...
Szymon OSTROWSKI (2005). Autocykliczny rozwój oksfordzkich bioherm gąbkowo-mikrobialitowych centralnej i południowej Polski. Volumina Jurassica, 3(1),
45-53. https://europub.co.uk./articles/-A-67866
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An overview of Yellow Limestone deposits of the Jaisalmer Basin, Rajasthan, India
Genesis of ferromanganese crusts in Jurassic pelagic limestones at Stankowa Skała, Pieniny Klippen Belt, Poland: sedimentological and petrological approach
The ferromanganese crusts (FMC) and nodules at Stankowa Skała near Nowy Targ (Pieniny Klippen Belt, Poland) are developed in pelagic condensed limestones. The crusts appear on an uneven surface of limestones with thinshe...
Kolonie korali z muszlowców ostrygowych i oolitów dolnego kimerydu Małogoszcza
Ammonite biostratigraphy in the Polish Jura sections (central Poland) as a clue for recognition of the uniform base of the Kimmeridgian Stage
The ammonite succession in the stratigraphical interval from the Bifurcatus Zone, through the Hypselum Zone, up to the lower part of the Bimammatum Zone corresponding to a large part of the Submediterranean Upper Oxfordi...
Architektura depozycyjna parasekwencji w utworach marginalno-morskich