The Clay and Závist faults ? one large strike-slip fault in the east part of Barrandian (Bohemian Massif)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00075391" target="_blank" >RIV/00216224:14310/14:00075391 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The Clay and Závist faults ? one large strike-slip fault in the east part of Barrandian (Bohemian Massif)

Popis výsledku v původním jazyce

The Clay and Závist faults are connected one another not only by the same direction but also by continuous change of their dip. The Clay Fault gradually changes its steep dipping to NW on the SW to subvertical orientation on the NE. Here, near Dobříš town, Závist Fault continuously varies analogously from subvertical position (on SW) to medium dipping to the SSE on the NE. It is obvious, that both faults are forming one single structure, whose surface is screwed into form of propeller. Construction of stratigraphy fault-cut (SFD) diagram was used to testify, whether faults movements are compatible (Fig. 1). Cross-cutting fault-cut lines indicate partially rotational nature of movement along the unified fault surface. The axis of rotation is projected to place near Dobříš town, where both walls of the fault take place in the Proterozoic sediments.

Název v anglickém jazyce

The Clay and Závist faults ? one large strike-slip fault in the east part of Barrandian (Bohemian Massif)

Popis výsledku anglicky

The Clay and Závist faults are connected one another not only by the same direction but also by continuous change of their dip. The Clay Fault gradually changes its steep dipping to NW on the SW to subvertical orientation on the NE. Here, near Dobříš town, Závist Fault continuously varies analogously from subvertical position (on SW) to medium dipping to the SSE on the NE. It is obvious, that both faults are forming one single structure, whose surface is screwed into form of propeller. Construction of stratigraphy fault-cut (SFD) diagram was used to testify, whether faults movements are compatible (Fig. 1). Cross-cutting fault-cut lines indicate partially rotational nature of movement along the unified fault surface. The axis of rotation is projected to place near Dobříš town, where both walls of the fault take place in the Proterozoic sediments.

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2014

Kód důvěrnosti údajů

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