Where is there chance to find deep prospects below the outer Western Carpathian thrust belt?

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F20%3A10246595" target="_blank" >RIV/61989100:27350/20:10246595 - isvavai.cz</a>

Alternative codes found

RIV/00216305:26110/20:PU138200

Result on the web

<a href="https://www.scopus.com/record/display.uri?eid=2-s2.0-85097990103&origin=resultslist#references" target="_blank" >https://www.scopus.com/record/display.uri?eid=2-s2.0-85097990103&origin=resultslist#references</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1088/1755-1315/609/1/012101" target="_blank" >10.1088/1755-1315/609/1/012101</a>

Result language

angličtina

Original language name

Where is there chance to find deep prospects below the outer Western Carpathian thrust belt?

Original language description

In the period of 80 and 90th, the intensive deep drilling and seismic profiling program in the Outer Western Carpathian belt has been realized for confirming the idea about the existence and opening of new promising plays beneath some of these thin-skinned belts. Many trans-Carpathian 2D seismic transects opened discussion on the understanding of the complex structure of thrust belts and its basement. The recent development of exploration, based on the new modern play concepts, has brought new light on this problem. The new 3D and the reprocessed 2D seismic sections from Czech and Slovak part of the Western Carpathian Flysch Belt disclosed several potentially new prospects, combined with the cover of the foreland of European plate. New significant reserves of hydrocarbons may occur in subthrust autochthonous and parautochthonous series buried below the frontal zones of thin-skinned thrust belts. The study of the deepest parts of the Carpathian Flysch belt has been based on the complex geochemical, structural analyses and geophysical Data reprocessing, supplied by verification along the chosen balanced sections. Four examples of 2D seismic transects, with registration up to 9-12 seconds, that present different tectonic style of structures of Flysch Belt and its platform basement, influenced by older large-scale faults, is presented from the western, northern and eastern parts of the Outer Western Carpathians. From point of view of hydrocarbon prospection, the most important features of the seismic profiles are the anticline structures of the North European Platform (NEP) below the thrust stack of the Flysch Belt. From the west to east the Týnec-Cunín, Drietoma, Orava and Zbudza elevations can be distinguished, created by a passive margin of the European plate, in the second and third structures probably by parautochthonous blocks of the same plate. (C) 2020 Institute of Physics Publishing. All rights reserved.

Czech name

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Czech description

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Type

D - Article in proceedings

CEP classification

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OECD FORD branch

10508 - Physical geography

Project

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Continuities

N - Vyzkumna aktivita podporovana z neverejnych zdroju

Publication year

2020

Confidentiality

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

Article name in the collection

IOP Conference Series: Earth and Environmental Science. Volume 609

ISBN

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ISSN

1755-1307

e-ISSN

1755-1315

Number of pages

9

Pages from-to

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Publisher name

IOP Publishing

Place of publication

Bristol

Event location

Praha

Event date

Sep 7, 2020

Type of event by nationality

WRD - Celosvětová akce

UT code for WoS article

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