Początek późnopaleozoicznego zlodowacenia Gondwany i jego zapis w polskich sukcesjach karbońskich

• Autorzy: Skompski S.

Warianty tytułu

EN

Onset of the late Palaeozoic Gondwanan glaciation and its sedimentary record in the Polish Carboniferous succession

• Języki publikacji: PL

Abstrakty

PL

Z porównania metod bezpośredniego i pośredniego datowania karbońskiego początku zlodowacenia Gondwany wynika, że najpewniejszym wskaźnikiem tego zdarzenia jest pojawienie się na południowym szelfie Laurussii specyficznego typu kontrolowanej glacieustatycznie sedymentacji cyklicznej. Spośród licznych obszarów tego szelfu z dobrze rozpoznanym zapisem sedymentacji względnie stabilne tektonicznie były obszary basenu lubelskiego i basenu Illinois (w przeciwieństwie np. do obszaru brytyjsko-belgijskiego i dnieprowsko-donieckiego). Analiza cykliczności w tych dwóch obszarach wskazuje, że początek zlodowacenia miał miejsce w brygancie (późny wizen). Wcześniejsza sedymentacja krótkookresowych cyklotemów (o przeciętnym okresie 100 000 lat), które pojawiły się w asbie, była prawdopodobnie wywołana przyczynami natury tektonicznej.

EN

Two specimens of Oslo rhomb porphyries find on the Wolin Island beach between Międzyzdroje and Grodno are extraordinary finds among the entire population of Scandinavian indicator erratics within glacial sediments in northern Poland. Only around 20 localities of erratics from Oslo have been noted in that part of Poland so far (Schulz, 1973). Unfortunately, the stratigraphy of the Wolin erratics is not known, because they have been found on the stony abrasion shelf at the foot of a cliff. The cliff itself consists of two separate till layers. The petrographical analysis of the lower bed of gray glacial till where rhomb porphyries had been found, point to distinctly north-western direction of an ice sheet advance (50 % of the entire population of erratics from sample 3 derive from western mother regions in the southern Baltic bottom). The analysed indicator erratics form the lower Wolin till represent the south-eastern Sweden and western part of the bottom of Baltic depression. The ice-sheet, approaching from the north, has transgressed on these outcrops before reaching the mother regions of Cretaceous limestones, which are located in the direct vicinity of the Wolin Island. The ample content of western erratics in sampled sediments of the Wolin cliff as well as the Oslo rhomb porphyries are of high interest. Have they come in icebergs (Benn & Evans, 1998, see Donner, 1995) or maybe their presence in glacial sediments should be connected with the Lagerlund's ice dome (1987, 1995)7 Schulz (2003) suggests a ship transport (as ballast stones). The planned detailed petrographical analysis on the Scandinavian erratics of the Wolin cliff should clarify the issue.

Słowa kluczowe

PL

cykliczność; dolny karbon; zlodowacenia; basen lubelski

EN

cyclicity; Lower Carboniferous; Gondwanan glaciations; Lublin Basin (E Poland)

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Przegląd Geologiczny
• Rocznik: 2003
• Tom: Vol. 51, nr 8
• Strony: 658--662
• Opis fizyczny: Bibliogr. 45 poz., wykr.

Twórcy

autor

Skompski S.

• Wydział Geologii, Uniwersytet Warszawski, ul. Żwirki i Wigury 93, 02-089 Warszawa,

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