Solution-collapse breccias in the upper Olenekian–Ladinian succession, Tatra Mts, Poland

Jaglarz, P.; Rychliński, T.

doi:10.14241/asgp.2018.020

Artykuł - szczegóły

Tytuł artykułu

Solution-collapse breccias in the upper Olenekian–Ladinian succession, Tatra Mts, Poland

Autorzy

Jaglarz P. , Rychliński T.

Treść / Zawartość

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Jaglarz_P_Solution_ASGP_Vol.88_No.4_2018.pdf

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DOI

10.14241/asgp.2018.020

Warianty tytułu

Języki publikacji

Abstrakty

The upper Olenekian-Middle Triassic succession of the Tatricum domain (Central Western Carpathians, southern Poland) includes a few horizons of breccias, which are intercalated with early-diagenetic dolostones. On the basis of macroscopic and microscopic (including cathodoluminescence) observations, the paper presents a new interpretation of the genesis of the breccias and their diagenetic history. The rocks studied range from monomictic, cemented mosaic packbreccias to chaotic, unsorted, monomictic, particulate rubble floatbreccias. The processes that preceded the formation of the breccias encompassed the precipitation of evaporites and the early-diagenetic dolomitization of lime muds. The solution-collapse breccias were formed during episodes of cyclic sediment emersions in the upper Olenekian and Middle Triassic, as the result of gradual sediment collapse after karstic dissolution of the intercalated evaporites. After the brecciation process, during diagenesis the rocks were subjected to cementation by sulphate minerals and next, to multi-stage dolomitization. Later tectonic processes led to fracturing and even re-brecciation of the previously formed solution-collapse breccias.

Słowa kluczowe

palaeokarst evaporites solution breccia dolomitization diagenesis Tatricum Triassic Western Carpathians

Wydawca

Polskie Towarzystwo Geologiczne

Czasopismo

Annales Societatis Geologorum Poloniae

Rocznik

2018

Tom

Vol. 88, No. 4

Strony

303--319

Opis fizyczny

Bibliogr. 66 poz., rys., tab.

Twórcy

autor

Jaglarz P.

piotr.jaglarz@uj.edu.pl

Jagiellonian University, Faculty of Geography and Geology, Institute of Geological Sciences, Gronostajowa 3a; 30-387 Kraków, Poland

autor

Rychliński T.

tomasz.rychlinski@uj.edu.pl

Jagiellonian University, Faculty of Geography and Geology, Institute of Geological Sciences, Gronostajowa 3a; 30-387 Kraków, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

Typ dokumentu

Bibliografia

Identyfikator YADDA

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