The Late Jurassic-Palaeogene Carbonate Platforms in the Outer Western Carpathian Tethys-A Regional Overview

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F21%3A10247976" target="_blank" >RIV/61989100:27350/21:10247976 - isvavai.cz</a>

Result on the web

<a href="https://www.mdpi.com/2075-163X/11/7/747" target="_blank" >https://www.mdpi.com/2075-163X/11/7/747</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3390/min11070747" target="_blank" >10.3390/min11070747</a>

Result language

angličtina

Original language name

The Late Jurassic-Palaeogene Carbonate Platforms in the Outer Western Carpathian Tethys-A Regional Overview

Original language description

The present work focuses on palaeogeographic reconstruction of shallow-water carbonate deposition in the Outer Western Carpathian Tethys. Platform deposits are preserved only as a component of turbidites and olistostromes, and reconstructions of these platforms are based on clastic material redistributed into slopes and deep basins and occurring among the Outer Carpathian nappes. Similar platforms were also present on the Tethys margins. These reconstructions were performed using the global models of plate tectonics. Several ridges covered by carbonate platforms developed in that area during the latest Jurassic-Palaeogene times. Three main shallow-water facies associations-Stramberk, Urgonian, and Lithothamnion-bryozoan-could be distinguished. The Tithonian-lowermost Cretaceous Stramberk facies is related to early, synrift-postrift stage of the development of the Silesian Domain. Facies that are diversified, narrow, shallow-water platforms, rich in corals, sponges, green algae, echinoderms, foraminifera, microencrusters, and microbes are typical of this stage. The Urgonian facies developed mainly on the south margin of the Outer Carpathian basins and is characterised by organodetritic limestones built of bivalves (including rudists), larger benthic foraminifera, crinoids, echinoids, and corals. Since the Paleocene, in all the Western Outer Carpathian sedimentary areas, Lithothamnion-bryozoan facies developed and adapted to unstable conditions. Algae-bryozoan covers originating on the siliciclastic substrate are typical of these facies. This type of deposition was preserved practically until the final stage in the evolution of the Outer Carpathian basins.

Czech name

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Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

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OECD FORD branch

10505 - Geology

Project

<a href="/en/project/GA20-10035S" target="_blank" >GA20-10035S: Leading edge instrumental methods in high resolution global Jurassic-Cretaceous boundary correlations</a><br>

Continuities

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year

2021

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Minerals

ISSN

2075-163X

e-ISSN

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Volume of the periodical

11

Issue of the periodical within the volume

7

Country of publishing house

CH - SWITZERLAND

Number of pages

26

Pages from-to

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UT code for WoS article

000676780200001

EID of the result in the Scopus database

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